Size: px
Start display at page:

Download ""

Transcription

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

16

17

18

19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

40

41

42

43

44

45

46

47

48

49

50

51

52

53

54

55 Kelemen et al. Fig N 55 N 50 N 190 W 180 W 170 W Komandorsky Komandorsky Islands dredge 70-B29 Attu Island Buldir Island BERING SEA Distal Aleutians Adak area Adak Island Atka Island block Amak Island Bogoslof Island Umnak Island Unalaska Island Western Aleutians Central Aleutians trench PACIFIC OCEAN 190 W 180 W Pacific - N. Am. 170 W convergence 60 N 55 N 50 N

56 Kelemen et al. Fig 2 lava samples number Kamchatka Straits dredges Piip, Komandorsky dredge 70-B29 Engenstrom depression Shemya (1) Attu, Agattu Buldir Kiska Semisopochnoi Little Sitkin, Segula Kanaga, Bobrof Atka Adak, Great Stikin Seguam Umnak Makushin, Unalaska Akutan Shishaldin, Unalaska Cold Bay longitude, W

57 Kelemen et al. Fig 3 70 molar Mg# > samples > 15 molar Mg# > molar Mg# > 0.6 wt% SiO wt% MgO 5 estimated temperature, C longitude, W longitude, W longitude, W lavas volcano averages 0.8 wt% SiO wt% MgO 15 5 molar Mg# longitude, W longitude, W longitude, W molar Mg# > molar Mg# > wt% FeO* wt% Na 2 O 4 2 wt% K 2 O molar Mg# > longitude, W longitude, W longitude, W wt% FeO* 5 wt% Na 2 O wt% K 2 O longitude, W longitude, W longitude, W 160

58 Kelemen et al. Fig 4 A east of Adak (gray) Adak area distal Aleutians, 177 to 187 W Komandorsky block Aleutian lavas Aleutian lavas Aleutian lavas east of Adak Adak west of Adak plus four samples with La/Yb < 1 wt% SiO 2 ppm K La/Yb molar Mg# B C , Aleutian plutons Aleutian plutons Aleutian plutons , Marianas lavas (open) Tanzawa plutonic complex (filled) 0.2 Marianas lavas (open) Tanzawa plutonic complex (filled) , Marianas lavas (open) Tanzawa plutonic complex (filled) molar Mg# molar Mg#

59 Kelemen et al. Fig 5A estimated continental crust (Mg# 0.45 to 0.54) samples wt% SiO 2 molar Mg# > wt% K 2 O molar Mg# > log(la/yb(n)) all data lavas Adak & west Komandorsky block distal Aleutians Adak, Kanaga, Bobrof lavas east of Adak plutons

60 Aleutians, west of Adak B29 5 Aleutians, west of Adak Aleutians, west of Adak B29 70B Kuriles Aleutians, east of Adak Kuriles Aleutians, east of Adak Kuriles 6 2 Aleutians, east of Adak Izu-Bonin/Mariana Lesser Antilles Izu-Bonin/Mariana Lesser Antilles Izu-Bonin/Mariana Lesser Antilles Tonga/Kermadec Scotia Tonga/Kermadec Scotia 20 Tonga/Kermadec 15 Scotia wt% SiO 2 reference line at 55 wt% average continental crust 59 wt% plots include lavas with molar Mg# > 0.5 wt% K 2 O reference line at 1 wt% average continental crust 1.9 wt% plots include lavas with molar Mg# > Pb/ 204 Pb plots include all lavas 5 Kelemen et al., figure 5b

61 Carlisle Amukta "Makushin, Unalaska Island" Bogoslof Komandorsky Straits Komandorsky Islands Piip volcano Komandorsky block distal Aleutians Adak area Atka & Seguam Rechesnoi volcano Umnak Island Okmok volcano Umnak Island concentration/morb concentration/morb concentration/morb Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Hf Sm Eu Gd Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni east central Aleutians Kelemen et al. figure 6 Figure 6, continued

62 Kelemen et al. figure 6A continental crust 0 Taylor & McL andesite model Taylor & McL bulk crust Taylor & McL Archean crust Weaver & Tarney bulk crust Rudnick & Fountain bulk crust concentration/morb Ba U Ta La Pb Sr Zr Sm Gd Ti Ho Tm Lu Co Th K Nb Ce Pr Nd Hf Eu Tb Dy Er Yb Y Ni

63 Kelemen et al. Fig lavas volcano averages Pb/ 204 Pb Sr/ 86 Sr Nd/ 144 Nd longitude, W

64 Kelemen et al. Fig updip convergence rate wt% SiO longitude, W convergence rate, m/yr samples > 15 wt% 12 wt% MgO 5 wt% FeO* convergence rate, m/yr convergence rate, m/yr wt% Na 2 O 3 2 wt% K 2 O convergence rate, m/yr convergence rate, m/yr

65 Kelemen et al. fig 9 KAMCHATKA GULF OF ALASKA 195 W 185 W 175 W 165 W 155 W 145 W W Kilometers OCEANIIC PELAGIC & HEMIPELAGIC SEDIMENT, DIATOM RICH; TRENCH-AXIS U-CRET-HOLO. TURBIDITE SEQUENCE, SIBERIAN DRAINAGES; QUAT? DISTAL TRENCH-AXIS TURBIDITE SEQUENCE, ALASKAN DRAINAGES; ~05. Myr OCEANIIC PELAGIC SEDIMENT, DIATOM RICH; EOCENE-QUAT. ZODIAK FAN TURBIDITE SEQUENCE, NORTH AMERICAN DRAINAGES; EOCENE-OLIG; Kodiak Seamount E ABYSSAL PLAIN TURBIDITE SEQUENCE; NORTH AMERICAN DRAINAGES; MIOC-HOLOCENE 8 Dead Kula-Pac Spreading Ridge? Ma Rat Fracture Zone Amlia Fracture Zone Ma Ma PACIFIC OCEANIC CRUST updip sediment thickness, meters updip sediment flux, m 3 /m/yr longitude, W longitude, W lavas volcano averages Pb/ 204 Pb Pb/ 204 Pb sediment flux, m 3 /m/yr sediment flux, m 3 /m/yr

66 Kelemen et al. Fig east of Adak Adak & west wt% MgO wt% SiO2 wt% TiO2 wt% Al2O wt% FeO* wt% CaO molar Mg# molar Mg# molar Mg# wt% Na2O wt% K2O temperature, C (1 bar, dry) + 3 samples > 15 wt%

67 Kelemen et al., figure lavas volcano averages DSDP 183 sediments 207 Pb/ 204 Pb Attu Adak avg 70B29 Adak EPR & JDF MORB Buldir Komandorsky block Pb/ 204 Pb DSDP 183 sediments Aleutian lavas volcano averages Attu Sr/ 86 Sr Sr/ 86 Sr Adak avg Komandorsky block Pb/ 204 Pb Pb/ 204 Pb Attu Adak avg Nd/ 144 Nd Komandorsky block 143 Nd/ 144 Nd Pb/ 204 Pb Pb/ 204 Pb

68 Kelemen et al., figure molar Mg# > lavas volcano averages 30 5 Th/Nb ppm Th ppm La longitude, W longitude, W Th/Nb Th/(Ta*17) volcano avg Th/Nb volcano avg Th/(Ta*17) molar Mg# > Ba/La Th/La La/Sm longitude, W lavas volcano averages longitude, W lavas volcano averages longitude, W longitude, W

69 Kelemen et al.,figure volcano averages east of Adak Adak & west 1 Elliott compilation east of Adak Adak & west 207 Pb/ 204 Pb Th/La Th/La 1 0 Ba/La volcano averages east of Adak Adak & west 1 Elliott compilaton 207 Pb/ 204 Pb Th/La Ba/La 1 0 Ba/La

70 Kelemen et al., figure lavas volcano averages Ba/Th longitude, W Sr/Nd molar Mg# > longitude, W 165 Ce/Pb longitude, W

71 Kelemen et al.,figure DSDP 183 sediments east of Adak Adak & west 15.6 Amak Bogoslof EPR & JDF MORB 207 Pb/ 204 Pb sed & MORB fluid? 70B29 Buldir 15.4 Komandorsky block Ce/Pb

72 1 0.8 sediment melt? eclogite melt? Ce/Pb 0 Kelemen et al., Figure 16 Th/La molar Mg# > 0.6 spinel peridotite source 00 eclogite melt? molar Mg# > eclogite melt? molar Mg# > low degree mantle melt Sr/Y high degree mantle melt wt% SiO 2 4 eclogite melt? sediment melt? Th/La Sr/Y Dy/Yb (N) 0 mantle component sediment melt? Th/Nb 00 molar Mg# > 0.6 eclogite melt? 0 low degree mantle melt high degree mantle melt wt% Na 2 O Sr/Y Sr/Y Dy/Yb (N) 00 eclogite melt? molar Mg# > mantle component La/Sm (N) 4 3 Dy/Yb (N) east of Adak Tb/Yb (N) east of Adak 3.5 Dy/Yb (N) Adak & west Tb/Yb (N) Adak & west eclogite melt? Ce/Pb Sr/Y Dy/Yb (N) 00 eclogite melt? eclogite melt? molar Mg# > wt% K 2 O Sr/Y Sr/Yb east of Adak Sr/9.6*Yb east of Adak Sr/Yb Adak & west Sr/9.6*Yb Adak & west east of Adak Adak & west

73 Kelemen et al., figure SiO 2 < 54 wt% 16 SiO 2 > 54 wt% 30 molar Mg# > < Mg# < La/Sm La/Sm

74 Kelemen et al., figure molar Mg# Nye & Reid ID1 Nye & Reid ID16 Nye & Reid ID18 Nye & Reid AS wt% SiO molar Mg# ,000 ppm K 0.6 molar Mg# La/Yb

75 Kelemen et al., figure Dy/Yb (N) east of Adak Tb/Yb (N) east of Adak Dy/Yb (N) Adak & west Tb/Yb (N) Adak & west 3 Dy/Yb(N) molar Mg#

76 Kelemen et al., figure 20 8 molar Mg# > 0.6 east of Adak Adak & west ppm Pb ppm Th

77 Kelemen at al., figure 21 melting of eclogite melting (MORB) of A garnet peridotite (pyrolite) B C % melting 1 % melting 2 % melting 5 % melting % melting % melting 20 % melting concentration/morb % melting 1 % melting 2 % melting 5 % melting % melting 20 % melting reaction consumes spinel peridotite produces garnet pyroxenite initial liquid 90 % liquid 80 % liquid 70 % liquid 60 % liquid 50 % liquid 40 % liquid 30 % liquid 20 % liquid % liquid concentration/morb concentration/morb reaction eclogite between melt & reaction between D E F spinel peridotite (pyrolite) spinel eclogite peridotite melt (abyssal) & 0 1 Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Sm Hf Gd Eu Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni initial liquid 1.25x liquid mass 1.5x liquid mass 2x liquid mass 3x liquid mass 0 1 Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Sm Hf Gd Eu Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni initial liquid 1.2x liquid mass 1.4x liquid mass 1.6x liquid mass 2x liquid mass 3x liquid mass concentration/morb concentration/morb 0.1 Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Sm Hf Gd Eu Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni reaction between eclogite melt & spinel peridotite (abyssal) initial liquid 3x liquid mass 5x liquid mass x liquid mass 20x liquid mass concentration/morb Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Sm Hf Gd Eu Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Sm Hf Gd Eu Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni Ba Th U K Ta Nb La Ce Pb Pr Sr Nd Zr Sm Hf Gd Eu Tb Ti Dy Ho Er Tm Yb Lu Y Co Ni

Along-Strike Trace Element and Isotopic Variation in Aleutian Island Arc Basalt: Subduction Melts Sediments and Dehydrates Serpentine

Along-Strike Trace Element and Isotopic Variation in Aleutian Island Arc Basalt: Subduction Melts Sediments and Dehydrates Serpentine University of South Florida Scholar Commons Geology Faculty Publications Geology 6-21-2007 Along-Strike Trace Element and Isotopic Variation in Aleutian Island Arc Basalt: Subduction Melts Sediments and

More information

Effect of tectonic setting on chemistry of mantle-derived melts

Effect of tectonic setting on chemistry of mantle-derived melts Effect of tectonic setting on chemistry of mantle-derived melts Lherzolite Basalt Factors controlling magma composition Composition of the source Partial melting process Fractional crystallization Crustal

More information

GSA Data Repository

GSA Data Repository GSA Data Repository 2015244 1. Method of Statistical Analysis Appendix DR1 One has to be careful and use only samples with complete Sm-Eu-Gd concentration data to study Eu/Eu* in the crust. This is because

More information

Supplementary Figure 1 Map of the study area Sample locations and main physiographic features of the study area. Contour interval is 200m (a) and 40m

Supplementary Figure 1 Map of the study area Sample locations and main physiographic features of the study area. Contour interval is 200m (a) and 40m Supplementary Figure 1 Map of the study area Sample locations and main physiographic features of the study area. Contour interval is 200m (a) and 40m (b). Dashed lines represent the two successive ridge

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO1250 Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation Takeshi Kuritani 1,2 *, Eiji Ohtani 1, and Jun-Ichi Kimura

More information

Melting Processes and Fluid and Sediment Transport Rates Along the Alaska-Aleutian Arc from an Integrated U-Th-Ra-Be Isotope Study

Melting Processes and Fluid and Sediment Transport Rates Along the Alaska-Aleutian Arc from an Integrated U-Th-Ra-Be Isotope Study University of South Florida Scholar Commons Geology Faculty Publications Geology 5-15-2003 Melting Processes and Fluid and Sediment Transport Rates Along the Alaska-Aleutian Arc from an Integrated U-Th-Ra-Be

More information

2 One View of the Geochemistry of Subduction-Related Magmatic Arcs

2 One View of the Geochemistry of Subduction-Related Magmatic Arcs 3.18 OneView of the Geochemistry of Subduction-Related Magmatic Arcs, with an Emphasis on Primitive Andesite and Lower Crust P. B. Kelemen Columbia University, Palisades, NY, USA K. HanghÖj Lamont-Doherty

More information

Supplementary Material

Supplementary Material Supplementary Material Machida et al. (214), Regional mantle heterogeneity regulates melt production along the Réunion hotspot-influenced Central Indian Ridge COMPILED DATA FOR THE RÉUNION HOTSPOT AND

More information

HP and UHP garnet peridotites and pyroxenites

HP and UHP garnet peridotites and pyroxenites HP and UHP garnet peridotites and pyroxenites Mantle wedge The least known piece of the subduction factory Mantle-wedge peridotites emplace within subducting continental crust (Brueckner, 998; van Roermund

More information

Supplementary Information

Supplementary Information Supplementary Information Crustal thickness control on Sr/Y signatures of recent arc magmas: an Earth scale perspective Massimo Chiaradia Section of Earth and Environmental Sciences, University of Geneva,

More information

An Introduction of Aleutian Subduction Zone. Chuanmao Yang, Hong Yang, Meng Zhang, Wenzhong Wang 2016/04/29

An Introduction of Aleutian Subduction Zone. Chuanmao Yang, Hong Yang, Meng Zhang, Wenzhong Wang 2016/04/29 An Introduction of Aleutian Subduction Zone Chuanmao Yang, Hong Yang, Meng Zhang, Wenzhong Wang 2016/04/29 Outline General Introduction Formation history Structure from seismic study geochemical features

More information

EMMR25 Mineralogy: Ol + opx + chlorite + cpx + amphibole + serpentine + opaque

EMMR25 Mineralogy: Ol + opx + chlorite + cpx + amphibole + serpentine + opaque GSA Data Repository 2017365 Marshall et al., 2017, The role of serpentinite derived fluids in metasomatism of the Colorado Plateau (USA) lithospheric mantle: Geology, https://doi.org/10.1130/g39444.1 Appendix

More information

Trace Elements. Today s lecture

Trace Elements. Today s lecture Trace Elements 300 Ni 200 ppm 100 0 300 Zr 200 100 0 40 50 60 70 80 SiO 2 wt. % Updates: M&M due date: Tuesday Today s lecture Topics: Trace element compositions Trace element behavior Partitioning Spider(

More information

GSA Data Repository

GSA Data Repository GSA Data Repository 218145 Parolari et al., 218, A balancing act of crust creation and destruction along the western Mexican convergent margin: Geology, https://doi.org/1.113/g39972.1. 218145_Tables DR1-DR4.xls

More information

Density assumed constant at 2800 kg/m3

Density assumed constant at 2800 kg/m3 Table 2 Volcanic Flux estimates Volcanic center or subset Volume Spacing Age Volume Mass Flux km 3 km Ma Fraction kg/m/ma Cosigüina 33 46 0.35 1 0.16 San Cristóbal 1 44 0.35 1 2.02 Telica (high U/La group)

More information

Summary of test results for Daya Bay rock samples. by Patrick Dobson Celia Tiemi Onishi Seiji Nakagawa

Summary of test results for Daya Bay rock samples. by Patrick Dobson Celia Tiemi Onishi Seiji Nakagawa Summary of test results for Daya Bay rock samples by Patrick Dobson Celia Tiemi Onishi Seiji Nakagawa October 2004 Summary A series of analytical tests were conducted on a suite of granitic rock samples

More information

} Institute of Volcanic Geology and Geochemistry, Petropavlovsk, Kamchatka , Russia

} Institute of Volcanic Geology and Geochemistry, Petropavlovsk, Kamchatka , Russia Magnesian andesite in the western Aleutian Komandorsky region: Implications for slab melting and processes in the mantle wedge G. M. Yogodzinski* Institute for the Study of the Continents and Department

More information

Composition of the Earth and its reservoirs: Geochemical observables

Composition of the Earth and its reservoirs: Geochemical observables Composition of the Earth and its reservoirs: Geochemical observables Cin-Ty A. Lee Rice University MYRES-I 2004 The Earth is dynamic and heterogeneous Atmosphere Midocean Ridge Plume Ocean Crust Oceanic

More information

DR Item Table DR1. Sample no Rock-type Oxide, wt% Trace Elements, ppm REE, ppm

DR Item Table DR1. Sample no Rock-type Oxide, wt% Trace Elements, ppm REE, ppm DR Item 2017318 for Sarıfakıoğlu, E., Dilek, Y., and Sevin, M., 2017, New synthesis of the Izmir-Ankara-Erzincan suture zone and the Ankara mélange in northern Anatolia based on new geochemical and geochronological

More information

Element Cube Project (x2)

Element Cube Project (x2) Element Cube Project (x2) Background: As a class, we will construct a three dimensional periodic table by each student selecting two elements in which you will need to create an element cube. Helpful Links

More information

XM1/331 XM1/331 BLFX-3 XM1/331

XM1/331 XM1/331 BLFX-3 XM1/331 a b AkC AkC strontian fluoro-apatite clinopyroxene phlogopite K-richterite XM1/331 clinopyroxene XM1/331 Fe-Ti ox c d clinopyroxene kric AkC ilmenite Sr-barite AkC XM1/331 BLFX-3 Supplementary Figure 1.

More information

THE MONTE MAGGIORE PERIDOTITE (CORSICA)

THE MONTE MAGGIORE PERIDOTITE (CORSICA) MONTE MAGGIORE CAPO CORSO CORSICA Giovanni B. Piccardo THE MONTE MAGGIORE PERIDOTITE (CORSICA) FIELD RELATIONSHIPS MORB Gabbro Spinel (ex-garnet) pyroxenites L ESCURSIONE A MONTE MAGGIORE The Monte Maggiore

More information

GSA DATA REPOSITORY

GSA DATA REPOSITORY GSA DATA REPOSITORY 2013011 Chen et al. ANALITICAL METHODS Microprobe analysis Microprobe analyses of minerals were done on a JEOL Superprobe JXA 8100 at the Key Laboratory of Orogenic Belts and Crustal

More information

February 20, Joe Cerniglia The International Group for Historic Aircraft Recovery (TIGHAR) Job Number: S0CHG688. Dear Joe:

February 20, Joe Cerniglia The International Group for Historic Aircraft Recovery (TIGHAR) Job Number: S0CHG688. Dear Joe: February 20, 2012 Joe Cerniglia The International Group for Historic Aircraft Recovery (TIGHAR) Subject: ICP-MS Report Job Number: S0CHG688 Dear Joe: Please find enclosed the procedure report for the analysis

More information

Overview of the KAHT system. Ian E.M. Smith, School of Environment, University of Auckland

Overview of the KAHT system. Ian E.M. Smith, School of Environment, University of Auckland Overview of the KAHT system Ian E.M. Smith, School of Environment, University of Auckland Tonga-Kermadec-New Zealand Arc Developed on the Pacific - Australian convergent margin Mainly intraoceanic except

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION DOI: 1.13/NGEO11 Deep-sea mud in the Pacific Ocean as a potential resource for rare-earth elements Yasuhiro Kato 1, Koichiro Fujinaga 1, Kentaro Nakamura, Yutaro Takaya 1, Kenichi

More information

The mantle metasomatism: diversity and impact What the mantle xenoliths tell us?

The mantle metasomatism: diversity and impact What the mantle xenoliths tell us? The mantle metasomatism: diversity and impact What the mantle xenoliths tell us? Mantle metasomatism Physical and chemical processes that are implemented during the flow of magmas and / or fluids within

More information

Worked Example of Batch Melting: Rb and Sr

Worked Example of Batch Melting: Rb and Sr Worked Example of Batch Melting: Rb and Sr Basalt with the mode: Table 9.2. Conversion from mode to weight percent Mineral Mode Density Wt prop Wt% ol 15 3.6 54 0.18 cpx 33 3.4 112.2 0.37 plag 51 2.7 137.7

More information

Breeding et al., Data Repository Material Figure DR1. Athens. Study Area

Breeding et al., Data Repository Material Figure DR1. Athens. Study Area Breeding, Ague, and Brocker 1 Figure DR1 21 o 24 Greece o A 38 o Athens Tinos 37 o Syros Attic-Cycladic Blueschist Belt Syros Kampos B Study Area Ermoupoli N Vari Unit Cycladic HP-LT Unit Marble horizons

More information

Subduction zones 3 arc magmatism

Subduction zones 3 arc magmatism 5. 3 Subduction zones 3 arc magmatism Where can we observe magmatic/volcanic activities along subduction zones? Characteristics of arc magmatism (vs. mid-ocean ridge/intraplate magmatism) Structure of

More information

Chapter 9: Trace Elements

Chapter 9: Trace Elements Lecture 13 Introduction to Trace Elements Wednesday, March 9, 2005 Chapter 9: Trace Elements Note magnitude of major element changes Figure 8-2. Harker variation diagram for 310 analyzed volcanic rocks

More information

Spot Name U-Pb ages (Ma) Plagioclase ages (Ma) Biotite age (Ma) Whole rock age (Ma)

Spot Name U-Pb ages (Ma) Plagioclase ages (Ma) Biotite age (Ma) Whole rock age (Ma) Table 1. Average U-Pb ages from this study in comparison with previous ages from Sherrod and Tosdal (1991, and references therein). Previous study ages are reported as ranges including uncertainty (i.e.

More information

SR Allen, RS Fiske, Y Tamura Sumisu methods

SR Allen, RS Fiske, Y Tamura Sumisu methods SR Allen, RS Fiske, Y Tamura Sumisu methods FTIR water contents from melt inclusions Quartz-hosted melt inclusions were analyzed for H 2 O and CO 2 by Fourier Transform Infrared Spectroscopy (FTIR) at

More information

Chapter 9: Trace Elements

Chapter 9: Trace Elements Chapter 9: Trace Elements Note magnitude of major element changes Figure 8.2. Harker variation diagram for 310 analyzed volcanic rocks from Crater Lake (Mt. Mazama), Oregon Cascades. Data compiled by Rick

More information

The Periodic Table. Periodic Properties. Can you explain this graph? Valence Electrons. Valence Electrons. Paramagnetism

The Periodic Table. Periodic Properties. Can you explain this graph? Valence Electrons. Valence Electrons. Paramagnetism Periodic Properties Atomic & Ionic Radius Energy Electron Affinity We want to understand the variations in these properties in terms of electron configurations. The Periodic Table Elements in a column

More information

Chemistry 431 Practice Final Exam Fall Hours

Chemistry 431 Practice Final Exam Fall Hours Chemistry 431 Practice Final Exam Fall 2018 3 Hours R =8.3144 J mol 1 K 1 R=.0821 L atm mol 1 K 1 R=.08314 L bar mol 1 K 1 k=1.381 10 23 J molecule 1 K 1 h=6.626 10 34 Js N A = 6.022 10 23 molecules mol

More information

Behaviour of high field strength elements in subduction zones: constraints from Kamchatka Aleutian arc lavas

Behaviour of high field strength elements in subduction zones: constraints from Kamchatka Aleutian arc lavas Earth and Planetary Science Letters 224 (2004) 275 293 www.elsevier.com/locate/epsl Behaviour of high field strength elements in subduction zones: constraints from Kamchatka Aleutian arc lavas Carsten

More information

Proposed draft marine bioregions

Proposed draft marine bioregions Proposed draft marine bioregions 1. PROPOSED PELAGIC BIOREGIONS Map 1. Proposed draft pelagic bioregions List of proposed pelagic bioregions: 1. Agulhas Current 2. Antarctic 3. Antarctic Polar Front 4.

More information

BONINITIC MELT INCLUSIONS IN CHROME SPINEL FROM THE OGASAWARA ARCHIPELAGO

BONINITIC MELT INCLUSIONS IN CHROME SPINEL FROM THE OGASAWARA ARCHIPELAGO GSA DATA REPOSITORY 2015057 BONINITIC MELT INCLUSIONS IN CHROME SPINEL FROM THE OGASAWARA ARCHIPELAGO DATA REPOSITORY for Thermal and chemical evolution of the subarc mantle revealed by spinel-hosted melt

More information

Geochemical analysis unveils frictional melting process in a

Geochemical analysis unveils frictional melting process in a GSA Data Repository 219116 1 2 3 Geochemical analysis unveils frictional melting process in a subduction zone fault Tsuyoshi Ishikawa and Kohtaro Ujiie 4 Supplemental Material 6 7 8 9 METHOD TABLES (Tables

More information

Solutions and Ions. Pure Substances

Solutions and Ions. Pure Substances Class #4 Solutions and Ions CHEM 107 L.S. Brown Texas A&M University Pure Substances Pure substance: described completely by a single chemical formula Fixed composition 1 Mixtures Combination of 2 or more

More information

Rare Earth Elements in some representative arc lavas

Rare Earth Elements in some representative arc lavas Rare Earth Elements in some representative arc lavas Low-K (tholeiitic), Medium-K (calc-alkaline), and High-K basaltic andesites and andesites. A typical N-MORB pattern is included for reference Notes:

More information

Lecture 25 Subduction Related Magmatism

Lecture 25 Subduction Related Magmatism Lecture 25 Subduction Related Magmatism Monday, May 2 nd 2005 Subduction Related Magmatism Activity along arcuate volcanic chains along subduction zones Distinctly different from the mainly basaltic provinces

More information

Supplementary material

Supplementary material Supplementary material Supplementary tables Bassis, A., Hinderer, M., Meinhold, G., Petrography and geochemistry of Palaeozoic quartz-rich sandstones from Saudi Arabia: implications for provenance and

More information

TABLE DR2. Lu-Hf ISOTOPIC DATA FOR WHOLE ROCK SAMPLES AND ZIRCONS [Lu] [Hf]

TABLE DR2. Lu-Hf ISOTOPIC DATA FOR WHOLE ROCK SAMPLES AND ZIRCONS [Lu] [Hf] TABLE DR1. LOWER CRUSTAL GRANULITE XENOLITH DERIVATION AND MINERALOGY Sample Kimberlite Type Mineralogy KX1-1 Lace s gt + qz + sa + rt (sil, ky, gr, su, cor, zr, mz) KX1-2 Lace s gt + sa + qz + rt (sil,

More information

Geological Assessment Report

Geological Assessment Report Wolverine Exploration Inc 5055 Mclean Rd. Quesnel, BC V2J 6C5 Geological Assessment Report Mineral Licenses: 012425M; 013039M; 013472M; 017521M Total 362 Claims NTS Map Sheets: 13E/Ol and 14F/04 Cache

More information

CLASS TEST GRADE 11. PHYSICAL SCIENCES: CHEMISTRY Test 4: Matter and materials 1

CLASS TEST GRADE 11. PHYSICAL SCIENCES: CHEMISTRY Test 4: Matter and materials 1 CLASS TEST GRADE PHYSICAL SCIENCES: CHEMISTRY Test 4: Matter and materials MARKS: 45 TIME: hour INSTRUCTIONS AND INFORMATION. Answer ALL the questions. 2. You may use non-programmable calculators. 3. You

More information

APPENDIX TABLES. Table A2. XRF analytical results for samples from drill hole AP5 (Areachap)

APPENDIX TABLES. Table A2. XRF analytical results for samples from drill hole AP5 (Areachap) APPENDIX TABLES Table A2. XRF analytical results for samples from drill hole AP5 (Areachap) Sample No. AP5/19 AP5/20 AP5/21 AP5/22 AP5/23 AP5/24 AP5/25AP5/26AP5/27AP5/28AP5/29AP5/30AP5/31AP5/32 AP5/33

More information

GSA DATA REPOSITORY

GSA DATA REPOSITORY GSA DATA REPOSITORY 2012161 Allan et al. SUPPLEMENTARY INFORMATION Summary of Magma Types Table DR1 summarizes some of the key petrologic, geochemical and physical characteristics of the three magma types

More information

Geology 103, Lab 07 Volcanoes

Geology 103, Lab 07 Volcanoes Geology 103, Lab 07 In lecture we have looked at different types of volcanoes and how tectonic processes such as seafloor spreading and subduction give rise to volcanic eruptions. In this lab you will

More information

Major and trace element composition of the high

Major and trace element composition of the high Article Volume 14, Number 8 22 August 2013 doi: ISSN: 1525-2027 Major and trace element composition of the high 3 He/ 4 He mantle: Implications for the composition of a nonchonditic Earth Matthew G. Jackson

More information

(C) Pavel Sedach and Prep101 1

(C) Pavel Sedach and Prep101 1 (C) Pavel Sedach and Prep101 1 (C) Pavel Sedach and Prep101 1 (C) Pavel Sedach and Prep101 2 (C) Pavel Sedach and Prep101 2 (C) Pavel Sedach and Prep101 3 (C) Pavel Sedach and Prep101 3 (C) Pavel Sedach

More information

Last 4 Digits of USC ID:

Last 4 Digits of USC ID: Chemistry 05 B Practice Exam Dr. Jessica Parr First Letter of last Name PLEASE PRINT YOUR NAME IN BLOCK LETTERS Name: Last 4 Digits of USC ID: Lab TA s Name: Question Points Score Grader 8 2 4 3 9 4 0

More information

Ch. 9 NOTES ~ Chemical Bonding NOTE: Vocabulary terms are in boldface and underlined. Supporting details are in italics.

Ch. 9 NOTES ~ Chemical Bonding NOTE: Vocabulary terms are in boldface and underlined. Supporting details are in italics. Ch. 9 NOTES ~ Chemical Bonding NOTE: Vocabulary terms are in boldface and underlined. Supporting details are in italics. I. Review: Comparison of ionic and molecular compounds Molecular compounds Ionic

More information

Atoms and the Periodic Table

Atoms and the Periodic Table Atoms and the Periodic Table Parts of the Atom Proton Found in the nucleus Number of protons defines the element Charge +1, mass 1 Parts of the Atom Neutron Found in the nucleus Stabilizes the nucleus

More information

What processes control the chemical compositions of arc front stratovolcanoes?

What processes control the chemical compositions of arc front stratovolcanoes? What processes control the chemical compositions of arc front stratovolcanoes? The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters

More information

Where are these melts generated in the mantle wedge?

Where are these melts generated in the mantle wedge? Melt generation processes in subduction zones T.L. Grove, C.B. Till, N. Chatterjee, E. Medard, S.W. Parman New experiments on H2O-saturated melting of mantle peridotite - The role of H2O in mantle wedge

More information

Martinique: a Clear Case for Sediment Melting andslabdehydrationasafunctionofdistance to the Trench

Martinique: a Clear Case for Sediment Melting andslabdehydrationasafunctionofdistance to the Trench JOURNAL OF PETROLOGY VOLUME 53 NUMBER PAGES^6 doi:.93/petrology/egs55 Martinique: a Clear Case for Sediment Melting andslabdehydrationasafunctionofdistance to the Trench SHASA LABANIEH *, CATHERINE CHAUVEL,AURE

More information

CHEM 10113, Quiz 5 October 26, 2011

CHEM 10113, Quiz 5 October 26, 2011 CHEM 10113, Quiz 5 October 26, 2011 Name (please print) All equations must be balanced and show phases for full credit. Significant figures count, show charges as appropriate, and please box your answers!

More information

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question.

MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. Geology 300, Physical Geology Spring 2019 Quiz Chapter 18, Seafloor Name MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. 1) Abyssal fans are made

More information

M10/4/CHEMI/SPM/ENG/TZ2/XX+ CHEMISTRY. Wednesday 12 May 2010 (afternoon) 45 minutes INSTRUCTIONS TO CANDIDATES

M10/4/CHEMI/SPM/ENG/TZ2/XX+ CHEMISTRY. Wednesday 12 May 2010 (afternoon) 45 minutes INSTRUCTIONS TO CANDIDATES M10/4/CHEMI/SPM/ENG/TZ/XX+ 106116 CHEMISTRY standard level Paper 1 Wednesday 1 May 010 (afternoon) 45 minutes INSTRUCTIONS TO CANDIDATES Do not open this examination paper until instructed to do so. Answer

More information

Be is produced by reactions of cosmic ray protons with N 2 and O 2 in the upper atmosphere

Be is produced by reactions of cosmic ray protons with N 2 and O 2 in the upper atmosphere 10 Be is produced by reactions of cosmic ray protons with N 2 and O 2 in the upper atmosphere 10 Be Be is a particle reactive element becomes concentrated in clayrich oceanic sediments 10 Be then undergoes

More information

Regional and local variations in geochemistry and tectonics along and across Central America

Regional and local variations in geochemistry and tectonics along and across Central America Regional and local variations in geochemistry and tectonics along and across Central America Michael J. Carr, Department of Geological Sciences, Wright Lab Rutgers University, 610 Taylor Rd., Piscataway

More information

Supplementary information

Supplementary information Supplementary information Sample details Samples used were from the Natural History Museum, London, UK: collections BM1968 P37 and BM1957 1056, and are listed in Supplementary Table1 and Table 2. Supplementary

More information

SEA-FLOOR SPREADING. In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:-

SEA-FLOOR SPREADING. In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:- SEA-FLOOR SPREADING In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:- Detailed bathymetric (depth) studies showed that there was an extensive submarine

More information

The Composition of the Continental Crust

The Composition of the Continental Crust The Composition of the Continental Crust Roberta L. Rudnick Geochemistry Laboratory Department of Geology University of Maryland Apollo 17 view of Earth Rationale: Why is studying crust composition important?

More information

Zircon/fluid trace element partition coefficients measured by recrystallization of Mud Tank zircon at 1.5 GPa and C

Zircon/fluid trace element partition coefficients measured by recrystallization of Mud Tank zircon at 1.5 GPa and C Zircon/fluid trace element partition coefficients measured by recrystallization of Mud Tank zircon at 1.5 GPa and 800-1000 C Tim Peters and John C. Ayers Vanderbilt University Funding by National Science

More information

Overview of the IBM Arc System: The Igneous Rocks

Overview of the IBM Arc System: The Igneous Rocks Overview of the IBM Arc System: The Igneous Rocks Robert J. Stern, Geosciences Department, University of Texas at Dallas, Box 830688, Richardson TX 75083-0688, U.S.A. rjstern@utdallas.edu The Izu-Bonin-Mariana

More information

Geochemical evolution of the Earth mantel and crust Part 1: Mantle geochemistry

Geochemical evolution of the Earth mantel and crust Part 1: Mantle geochemistry Geochemical evolution of the Earth mantel and crust Part 1: Mantle geochemistry Mantel geochemistry Snæfellsjökull, Iceland Stromboli, Sicily Recommended reading Allègre, J.C. (2008) Isotope Geology, Cambridge

More information

Geochemistry of Permian rocks of the Yukon-Tanana terrane, western Yukon: GEM 2 Cordillera project

Geochemistry of Permian rocks of the Yukon-Tanana terrane, western Yukon: GEM 2 Cordillera project GEOLOGICAL SURVEY OF CANADA OPEN FILE 8170 Geochemistry of Permian rocks of the Yukon-Tanana terrane, western Yukon: GEM 2 Cordillera project D. Milidragovic, J.J. Ryan, A. Zagorevski, S.J. Piercey 2016

More information

8. Relax and do well.

8. Relax and do well. CHEM 1215 Exam III John III. Gelder November 11, 1998 Name TA's Name Lab Section INSTRUCTIONS: 1. This examination consists of a total of 7 different pages. The last page includes a periodic table and

More information

An Igpet Gallery July 4, 2014

An Igpet Gallery July 4, 2014 An Igpet Gallery July 4, 214 DI Fuego Santa Ana Masaya OL Opx SIL 3 Fuego Santa Ana Masaya 2 K 2 O 1 5 6 Regression lines are sometimes informative and colored backgrounds can be either soothing or distracting.,

More information

8. Relax and do well.

8. Relax and do well. CHEM 1515 Exam II John II. Gelder October 14, 1993 Name TA's Name Lab Section INSTRUCTIONS: 1. This examination consists of a total of 8 different pages. The last two pages include a periodic table, a

More information

Guide to the Extended Step-Pyramid Periodic Table

Guide to the Extended Step-Pyramid Periodic Table Guide to the Extended Step-Pyramid Periodic Table William B. Jensen Department of Chemistry University of Cincinnati Cincinnati, OH 452201-0172 The extended step-pyramid table recognizes that elements

More information

Table 1: Summary of petrographic characteristics for porphyritic samples from Campbell and Chatham islands, New Zealand phenocrysts sample location

Table 1: Summary of petrographic characteristics for porphyritic samples from Campbell and Chatham islands, New Zealand phenocrysts sample location Table 1: Summary of petrographic characteristics for porphyritic samples from Campbell and Chatham islands, New Zealand phenocrysts sample location deposit type rock type age/unit >5%

More information

Evidence for and implications of a Bering plate based on geodetic measurements from the Aleutians and western Alaska

Evidence for and implications of a Bering plate based on geodetic measurements from the Aleutians and western Alaska JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113,, doi:10.1029/2007jb005136, 2008 Evidence for and implications of a Bering plate based on geodetic measurements from the Aleutians and western Alaska Ryan S. Cross

More information

(please print) (1) (18) H IIA IIIA IVA VA VIA VIIA He (2) (13) (14) (15) (16) (17)

(please print) (1) (18) H IIA IIIA IVA VA VIA VIIA He (2) (13) (14) (15) (16) (17) CHEM 10113, Quiz 3 September 28, 2011 Name (please print) All equations must be balanced and show phases for full credit. Significant figures count, show charges as appropriate, and please box your answers!

More information

Made the FIRST periodic table

Made the FIRST periodic table Made the FIRST periodic table 1869 Mendeleev organized the periodic table based on the similar properties and relativities of certain elements Later, Henri Moseley organized the elements by increasing

More information

IV. Governador Valadares clinopyroxenite, 158 grams find

IV. Governador Valadares clinopyroxenite, 158 grams find IV. Governador Valadares clinopyroxenite, 158 grams find Figure IV-1. Photograph of Governador Valadares (158 grams) from Dr. Fernanda Ferrucci via Dr. Giuseppe Cavarretta. Photo taken by L. Spinozzi.

More information

Introduction to Earth s s Spheres The Benchmark

Introduction to Earth s s Spheres The Benchmark Introduction to Earth s s Spheres The Benchmark Volcanism Volcanic eruptions Effusive: lavas (e.g., Kilauea) Volcanism Volcanic eruptions Explosive: pyroclastic rocks (e.g., Krakatau) Factors Governing

More information

The Periodic Table of Elements

The Periodic Table of Elements The Periodic Table of Elements 8 Uuo Uus Uuh (9) Uup (88) Uuq (89) Uut (8) Uub (8) Rg () 0 Ds (9) 09 Mt (8) 08 Hs (9) 0 h () 0 Sg () 0 Db () 0 Rf () 0 Lr () 88 Ra () 8 Fr () 8 Rn () 8 At (0) 8 Po (09)

More information

Chapter 3: Stoichiometry

Chapter 3: Stoichiometry Chapter 3: Stoichiometry Chem 6A Michael J. Sailor, UC San Diego 1 Announcements: Thursday (Sep 29) quiz: Bring student ID or we cannot accept your quiz! No notes, no calculators Covers chapters 1 and

More information

CHM 101 PRACTICE TEST 1 Page 1 of 4

CHM 101 PRACTICE TEST 1 Page 1 of 4 CHM 101 PRACTICE TEST 1 Page 1 of 4 Please show calculations (stuffed equations) on all mathematical problems!! On the actual test, "naked answers, with no work shown, will receive no credit even if correct.

More information

02/05/09 Last 4 Digits of USC ID: Dr. Jessica Parr

02/05/09 Last 4 Digits of USC ID: Dr. Jessica Parr Chemistry 05 B First Letter of PLEASE PRINT YOUR NAME IN BLOCK LETTERS Exam last Name Name: 02/05/09 Last 4 Digits of USC ID: Dr. Jessica Parr Lab TA s Name: Question Points Score Grader 2 2 9 3 9 4 2

More information

The Genesis of Kurišková U-Mo ore deposits. Rastislav Demko, Štefan Ferenc, Adrián Biroň, Ladislav Novotný & Boris Bartalský

The Genesis of Kurišková U-Mo ore deposits. Rastislav Demko, Štefan Ferenc, Adrián Biroň, Ladislav Novotný & Boris Bartalský The Genesis of Kurišková U-Mo ore deposits Rastislav Demko, Štefan Ferenc, Adrián Biroň, Ladislav Novotný & Boris Bartalský Kurišková project development Uranium (uranium ore) has higher value in comparison

More information

[ ]:543.4(075.8) 35.20: ,..,..,.., : /... ;. 2-. ISBN , - [ ]:543.4(075.8) 35.20:34.

[ ]:543.4(075.8) 35.20: ,..,..,.., : /... ;. 2-. ISBN , - [ ]:543.4(075.8) 35.20:34. .. - 2-2009 [661.87.+661.88]:543.4(075.8) 35.20:34.2373-60..,..,..,..,.. -60 : /... ;. 2-. : -, 2008. 134. ISBN 5-98298-299-7 -., -,,. - «,, -, -», - 550800,, 240600 «-», -. [661.87.+661.88]:543.4(075.8)

More information

N = N 0 e -λt D* = N 0 -N D* = N 0 (1-e -λt ) or N(e λt -1) where N is number of parent atoms at time t, N 0

N = N 0 e -λt D* = N 0 -N D* = N 0 (1-e -λt ) or N(e λt -1) where N is number of parent atoms at time t, N 0 N = N 0 e -λt D* = N 0 -N D* = N 0 (1-e -λt ) or N(e λt -1) where N is number of parent atoms at time t, N 0 is initial number of parents, D* is number of radiogenic daughter atoms, and λ is the decay

More information

TRACE ELEMENT ANALYSIS OF DIAMOND BY LAM ICPMS: STANDARDISATION, RESULTS AND DIRECTIONS

TRACE ELEMENT ANALYSIS OF DIAMOND BY LAM ICPMS: STANDARDISATION, RESULTS AND DIRECTIONS TRACE ELEMENT ANALYSIS OF DIAMOND BY LAM ICPMS: STANDARDISATION, RESULTS AND DIRECTIONS W.L. Griffin 1, 3, Sonal Rege 1, Rondi M. Davies 1, 2, Simon Jackson 1, Suzanne Y. O Reilly 1 1.ARC National Key

More information

Melt inclusions from Marianas arc lavas: implications for the composition and formation of island arc magmas

Melt inclusions from Marianas arc lavas: implications for the composition and formation of island arc magmas Chemical Geology 183 (2002) 263 286 www.elsevier.com/locate/chemgeo Melt inclusions from Marianas arc lavas: implications for the composition and formation of island arc magmas Adam J.R. Kent a, *, Tim

More information

PHYSICAL SCIENCES GRADE : 10

PHYSICAL SCIENCES GRADE : 10 PHYSICAL SCIENCES GRADE : 0 TIME : hour TOTAL : 75 INSTRUCTIONS AND INFORMATION. Write your full name on your answer book in the appropriate place. 2. The question paper consists of SEVEN questions. Answer

More information

Plates Moving Apart Types of Boundaries

Plates Moving Apart Types of Boundaries Plates Moving Apart Types of Boundaries PLATE TECTONICS IS The theory that the Earth s crust is broken into slabs of rock that move around on top of the asthenosphere. How fast are plates moving? The Arctic

More information

Backarc origin of Neoarchean metamorphism and orogenic root growth

Backarc origin of Neoarchean metamorphism and orogenic root growth GSA Data Repository 2017 Backarc origin of Neoarchean metamorphism and orogenic root growth ultrahigh temperature Gregory Dumond, Michael L. Williams, Michael J. Jercinovic, Julia A. Baldwin Analytical

More information

OCN 201 Physiography of the Seafloor

OCN 201 Physiography of the Seafloor OCN 201 Physiography of the Seafloor 1 Ocean Depth versus Continental Height Why do we have dry land? Solid surface of Earth is dominated by two levels: Land with a mean elevation of +840 m (29% of Earth

More information

NAME: FIRST EXAMINATION

NAME: FIRST EXAMINATION 1 Chemistry 64 Winter 1994 NAME: FIRST EXAMINATION THIS EXAMINATION IS WORTH 100 POINTS AND CONTAINS 4 (FOUR) QUESTIONS THEY ARE NOT EQUALLY WEIGHTED! YOU SHOULD ATTEMPT ALL QUESTIONS AND ALLOCATE YOUR

More information

Circle the letters only. NO ANSWERS in the Columns! (3 points each)

Circle the letters only. NO ANSWERS in the Columns! (3 points each) Chemistry 1304.001 Name (please print) Exam 4 (100 points) April 12, 2017 On my honor, I have neither given nor received unauthorized aid on this exam. Signed Date Circle the letters only. NO ANSWERS in

More information

ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017

ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 Why is there no oceanic crust older than 200 million years? SUBDUCTION If new oceanic crust is being continuously created along the earth

More information

Chapter 02 The Sea Floor

Chapter 02 The Sea Floor Chapter 02 The Sea Floor Multiple Choice Questions 1. One of the following is not one of the world's major ocean basins: A. Atlantic Ocean B. Arctic Ocean C. Indian Ocean D. Antarctic Ocean E. Pacific

More information

Chemistry 2 Exam Roane State Academic Festival. Name (print neatly) School

Chemistry 2 Exam Roane State Academic Festival. Name (print neatly) School Name (print neatly) School There are fifteen question on this exam. Each question is weighted equally. n the answer sheet, write your name in the space provided and your answers in the blanks provided.

More information

Trace elements in clinopyroxenes from Aleutian xenoliths: Implications for primitive subduction magmatism in an island arc

Trace elements in clinopyroxenes from Aleutian xenoliths: Implications for primitive subduction magmatism in an island arc Earth and Planetary Science Letters 256 (2007) 617 632 www.elsevier.com/locate/epsl Trace elements in clinopyroxenes from Aleutian xenoliths: Implications for primitive subduction magmatism in an island

More information

Spin Cut-off Parameter of Nuclear Level Density and Effective Moment of Inertia

Spin Cut-off Parameter of Nuclear Level Density and Effective Moment of Inertia Commun. Theor. Phys. (Beijing, China) 43 (005) pp. 709 718 c International Academic Publishers Vol. 43, No. 4, April 15, 005 Spin Cut-off Parameter of Nuclear Level Density and Effective Moment of Inertia

More information