New Mexico Bureau of Mines & Mineral Resources Socorro. NM 87801
|
|
- Felicity Young
- 5 years ago
- Views:
Transcription
1 New Mexico Bureau of Mines & Mineral Resources Socorro. NM 8781 A DIVISION OF NEW MEICO INSTITUTE OF MINING & TECHNOLOGY OP,ENFILE REPORT 286 HYDROCARBON SOURCE ROCK EVALUATION OF ODESSA NATURAL GAS CORPORATION, NO. 3 w. s. RANCH SEC. 24, T29N, R19E, COLFA COUNTY, NEW MEICO BY Geoffrey S. Bayliss and Rudy R. Schwarzer June 1987 NEW MEICO TECH IS AN EWAL OPPOATVNITYIAFFIRMATNE ACTION INSTITUTION
2 NEW MEICO HYJJROCARBON SOURCE ROCK EVALUATION PROJECT ODESSA NATURAL GAS CORPOWTION, H.3 W.S. BAACA SEC. 24, T29N, R19E, COLFA COUNTY, NEW MEICO API NO NORTHEAST AREA GEOCHEM JOB NO Prepared for PROGRAM PARTICIPANTS Dr. Geoffrey S. Bayliss and Dr. Rudy R. Schwarzer GEOCHEM LABORATORIES, INC. 1143C BRITTMOORE ROAD HOUSTON, TEAS 7743 (713) CONFIDENTIAL JUNE, 1987
3 NEW MEICO HYDROCARBON SOURCE ROCK EVALUATION WELL NAME: API NO.: AREA: LOCATION: GEWHEM JOB NO. : TOTAL DEPTH: INTERVAL SAMPLED: TOTAL NUMBER OF SAMPLES: ODESSA NATURAL GAS CORPORATION, N.3 W.S. RANC NORTHEAST COLFA COUNTY, NEW MEICO SEC.24, T29N, R19E ft ft. 11 GEOCHEM SAMPLE NUMBER SAMPLE DEPTH STRATlGRAPHIC INTERVAL f B H cl U H E Lh E I Verne j o?ierre?ierre?ierre?ierre?ierre 'liobrara 'liobrara 2arlile keenhorn kaneros L
4 ~ ~ ~ ~ "" ~... w 1IL 3 c3 H LL w hl h k LL I I I 1 I I 1 I I1 I 1 I I I I1 I I I I b """""""""""~""""~"~ hl I,, I I I I I, I Ln W O N OLT LL I I I 1 II I I I I cu """""""""""~"""""" " I I I I I I I ' L r u I I 1 I Ln "... Ln 4 u "_.... ~ W ~... a ae """"" I" """""q==~z=r=~===~=====~=======~==~==="""" 3LwLL"" x ~""""""""""""""""""""""""""" Urn z t+y 3 " ""_""_ I ll I I I 1 ~. I ),, hl Ln h E v 4 I Ln Ln cn I I II I I I I " cn 4 \ """~"""""""""""""""""""""""" N v, ""_ """""""""""" """"" "" """ 3 I,t, I I I I, H CI I I I I I I I I I,, I!, I,, a _""""""""""""""""~ """"""""""~""""""~ I I! I II I I I I., a " I ae """""""""""""""""""" I,,I I I I, I I,,,,, d" Ln
5 ~ ~ ~~~~~~ ~ TABLE I RESULTS OF TOTAL ORGANIC CARBON NEW MEICO HYDROCARBON SOURCE ROCK EVALUATION ODESSA NATURAL GAS CORP., N.3 W.S. RANCH SEC.24, T29N, R19E, COLFA COUNTY, NEW MEICO API #3725 GEOCHEM SAMPLE NUMBER DEPTH INTERVAL (feet) TOTAL ORGANIC CARBON (% of Rock) /1.71
6 TABLE I1 LITEOLOGICAL DESCRIPTIONS AND ORGANIC CARBON ANALYSES NEW MEICO HYDROCARBON SOURCE ROCK EVALUATION ODESSA NATURAL GAS CORP., N.3 W.S. RANCH SEC.24, T29N, R19E, COLFA COUNTY, NEW MEICO API GEOCHEM DEPTE. SAMPLE INTERVAL NUMBER (feet) DESCRIPTION LITHO GSA NO. ORGANIC CARBON (Wt A % Mudstone, dark gray. N A % Mudstone, dark gray. N A % Mudstone, slightly calcareous, dark gray. N A % Mudstone, dark gray. N3 1.17/ A % Mudstone, dark gray. N A % Mudstone, dark gray. N A % Mudstone, calcareous, dark gray. N A % Mudstone, calcareous, dark gray. N A % Mudstone, dark gray. N A % Mudstone, very calcareous, dark gray. N A % Mudstone, dark gray. ' N3 1.59/1.71
7 TABLE Ill SRY OF ORGANIC CARBON AND VISUAL KEROGEN DATA NEW MEICO HYDROCARBON SOURCE ROCK EVALUATION ODESSA NATURAL GAS CORP.. N.3 W.S. RANCH SEC.24, n9n, U9E, COLFA~COUNTY, NEW MEICO API #3D725 GEOCBW slb IRR(BER ~..~." TUTAL ORGANIC CARBON l ORGANIC I U R TYPE RW;I;A EW;I;A H:Wl:A W1;E; W1;H;A A;*; Wl;H;A T I T VIS L ABLBURDANCE NORM T A " [ZED PERCENT to 2+ 2 to 2+ 2 to 2+ 2 to 2+ 2 to to 3 2+ to 3 2+ to I., LEGEND: KEROGEN KEY Predoinant; Secondary; Trace 'r9? 929? A1 = A = A* = A = H* w u I = c Algal AorphousSepropel Relic AorphousSapropel HerbaceousSporeleollen Degraded Herbaceous WoodyStructured Unidentified Material lnertinite cos1y
8 TULE 1V RLISLlLTS OF ROCKSVN, PYROLYSlS MALYSIS NEW MElCO HYOROCARBON SOURCE ROCK EVALUATION ODESSA NATURAL GAS COUP., N.3 W.S. RANCR SEC.24, T29N, R19E, COLFAF. COUNTY, NEW MElCO APl Q I T.O.C. = Total orpanic carbon, vt.% 53 = co2 produced fro kerogen pyrolysis Oxygen s1 Frea hydrocarbons, g Aclg of rock (w CO2/g of rock) Index g CO21g organic carbon 52 = Residual hydrocarbon potential P F.83 (SI + 92) PI = SIISI + 52 (g HClg or Aydropen rock) TMA lndex Teperature Index, degreea C. g HC/p orgenic carbon
9
10 ~ LEGEND FOR SUMMARY DIAGFAM DEPTH : LITHO LOG: STRATIGRAPHY: % TOC: AI : 1 : HC YIELD: ZJZir KEROGEN: TMA : %ROA): rn FREE HC: PI: in feet see lithology sybols by age percent total organic carbon RockEval, Hydrocarbon Index = 1 S2(/ Wt)/TOC RockEval, Oxygen Index = 1 S3 (O/OO Wt)/TOC RockEval, S2 peak (pp) RockEval, Ratio of S2 to 53 peak see Kerogen sybols RockEval, axiu teperature of S2 peak, in degrees Centigrade Vitrinite Reflectance (scale to 5) Theral Alteration Index (Scale to 1 5) RockEval, S1 peak (pp) RockEval, Productivity Index = Sl/(SI+S2) LITHOLOGIES KEROGEN TYPES 11 SHALE SILICEOUS ROCKS 1 b MUDSTONE EVAPORITES SILTSTONE ' SANDSTONE COAL IGNEOUS ROCKS... AMORPHOUS HERBFlCEOUS WOOD" INERTINITE CONGLOMERATE BRECCIA VOLCRNICS ROCKS METAMORPHIC LIMESTONE DOLOMITE BRSEMENT OTHER E] RL D<I MISSING SECTION
11 APPEMID( A
12 GEOTHERMAL DIAGENETIC CRITERIA (QWEY uaw. 8w.1
by L. Paul Tybor New Mexico Bureau of Mines and Mineral Resources Open File Report No. OF 197
New Mexico Bureau of Mines and Mineral Resources Open File Report No. OF 197 HYDROCARBON SOURCE-ROCK EVALUATION STUDY, COCKRELL NO. 1 STATE-11349 WELL LUNA COUNTYl NEW MEXICO GeoChern Laboratories, Inc.
More informationTABLE
ORGANIC CARBON RESULTS TABLE 1 5; TABLE 1677-013 1677-014 1677-015 1677-016 TABLE 1 ORGANIC CARBON RESULTS AND GROSS LJTHOLOGIC DESCRIPTIONS GEOCHEM G S A TOTAL ORGANIC SAMPLE NUMBER DEPTH GROSS LITHOLOG1C
More informationDOYA ANA COUNTY, NEW MEXICO
New Mexico Bureau of Mines and Mineral Resources Open File Report No. OF 201 HYDROCARBON SOURCE-ROCK EVALUATION STUDY, SINCLAIR NO. 1 DOGA ANA FEDERAL 18 WELL DOYA ANA COUNTY, NEW MEXICO by Douglas A.
More informationby Ann Brooke Reaugh and Douglas A. Muckelroy GeoChem Laboratories, Inc. Houston, Texas
New Mexico Bureau of Mines and Mineral Resources Open File Report No. OF-348 ORGANIC GEOCHEMICAL ANALYSES OF THE MERRION OIL AND GAS C3RP. NO. 1 ARENA BWCA WELL, MCKINLEY COUNTY, NEW MEXICO by Ann Brooke
More informationNew Mexico Bureau of Mines and Mineral Resources Open File Report No. OF-205
New Mexico Bureau of Mines and Mineral Resources Open File Report No. OF-205 ORGANIC GEOCHEMICkL ANALYSIS, PURE NO. 1 FEDERAL H WELL, DONA ANA COUNTY, NEW MEXICO by Stephen R. Jacobson, James S. Rankin
More informationPETROLEUM GEOCHEMISTRY REPORT PREPARED FOR NORSK HYDRO. Geochemical Evaluation of Sediments from Well: 7/11-8.
GEOCHEWCAL CONSU V/.N" S COMPANY INCORPORATED IN U.K. NO. 1509402 VAT REGISTRATION NO. 354021394 UNIT 14, PARAMOUNT INDUSTRIAL ESTATE, SANDOWN ROAD, WATFORD WD2 4XA. TEL: 43196/31416 TELEX: 8812973. *
More informationGEOCHEMICAL EVALUATION AND HYDROCARBON CHARACTERISATION STUDY 6406 EXECUTE SUMMARY
GEOCHEMICAL EVALUATION AND HYDROCARBON CHARACTERISATION STUDY 6406 WC bla EXECUTE SUMMARY The section between 600 metres and 4520 metres has 1987 REGISTRERT OUEDIREKTORATET hrrn nvrnluntrrt. Apart from
More informationPyrolysis and TOC Identification of Tight Oil Sweet Spots TALK OUTLINE
Pyrolysis and TOC Identification of Tight Oil Sweet Spots Albert Maende* and W. David Weldon, Wildcat Technologies, LLC, Humble, TX, United States. TALK OUTLINE Formation area of study Type of data, analytical
More informationThe Shale Spectrum: Interdisciplinary understanding across oil shale, oil-bearing shale and gas shale plays
The Center for Oil Shale Technology & Research & The Colorado School of Mines 31sᵗOil Shale Symposium October 17-21, 2011 at the Cecil H. & Ida Green Center, Colorado School of Mines, Golden, Colorado
More information22. PETROLEUM-GENERATING POTENTIAL OF SEDIMENTS FROM LEG 44, DEEP SEA DRILLING PROJECT
. PETROLEUM-GENERATING POTENTIAL OF SEDIMENTS FROM LEG, DEEP SEA DRILLING PROJECT J.W. Kendrick, A. Hood, and J.R. Castano, Shell Development Company, Houston, Texas ABSTRACT The abundance, type, and thermal
More informationRelationships of the Ordovician. Appalachian Basin. June 21, 2011
Regional Stratigraphic and Facies Relationships of the Ordovician Utica/Point i t Pleasant Interval in the Appalachian Basin June 21, 2011 Ron Riley and Mark Baranoski Stratigraphic Correlation Chart Modified
More informationSedimentary Rocks, Stratigraphy, and Geologic Time
Sedimentary Rocks, Stratigraphy, and Geologic Time A rock is any naturally formed, nonliving, coherent aggregate mass of solid matter that constitutes part of a planet, asteroid, moon, or other planetary
More informationDawsonite breakdown reactions during pyrolysis in Green River Formation oil shale
Dawsonite breakdown reactions during pyrolysis in Green River Formation oil shale Jeremy Boak, Colorado School of Mines Justin Birdwell, U. S. Geological Survey Outline Saline Minerals in Green River Formation
More informationPage 1. Name:
Name: Questions 1 through 3 refer to the following: The diagrams below represent two rock outcrops found several miles apart in New York State. Individual rock layers are lettered, and fossils and rock
More informationTABLE 2 ORGANIC CARBON RESULTS AND GROSS LITHOLOGIC DESCRIPTIONS
ORGANIC CARBON RESULTS TABLE 2 ORGANIC CARBON RESULTS TABLE 2 TABLE TABLE 2 ORGANIC CARBON RESULTS AND GROSS LITHOLOGIC DESCRIPTIONS GEOCHEM SAMPLE NUMBER DEPTH GROSS LITHOLOGIC DESCRIPTION GS A Colour
More informationPage 1. Name: Period: Date: WS Metamorphic Rocks. The diagram below represents a rock with a distorted layer structure.
Name: Period: Date: 9317-1 - Page 1 WS Metamorphic Rocks 1) The diagram below represents a rock with a distorted layer structure. 5) Which rock is most likely a nonsedimentary rock? A) a rock showing mud
More information1 Hfli. ^^Hi. 11 mw\i. mmsisi i lull I. IMMRrtHttiifHmiititlK. RibWh. llml ''.' 1 ffililsiillsll8 ill. iiiinitsim IK«
l i. :,, v. i :! 1.» r =,
More informationOrganic Richness J. W. KENDRICK, A. HOOD, J. R. CASTANO. VITRINITE REFLECTANCE (CASTANO, IN HOOD and CASTANO, 1974)
. PETROLEUM-GENERTING POTENTIL OF SEDIMENTS FROM LEG 0, DEEP SE DRILLING PROJECT J. W. Kendrick,. Hood, and J. R. Castano, Shell Development Company, Bellaire Research Center, Houston, Texas INTRODUCTION
More informationURANIUM RESOURCES IN NEW MEXICO. Virginia T. McLemore New Mexico Bureau of Geology and Mineral Resources, New Mexico Tech, Socorro, NM
URANIUM RESOURCES IN NEW MEXICO Virginia T. McLemore New Mexico Bureau of Geology and Mineral Resources, New Mexico Tech, Socorro, NM Purpose Describe the uranium industry in New Mexico, with emphasis
More informationExploration / Appraisal of Shales. Petrophysics Technical Manager Unconventional Resources
Exploration / Appraisal of Shales Rick Lewis Petrophysics Technical Manager Unconventional Resources Organic Shale Factors Controlling Gas Reservoir Quality Conventional sandstone Mineral framework Gas
More information21. GEOCHEMICAL ANALYSIS OF SAMPLES FROM SITES 397 AND 398
21. GEOCHEMICAL ANALYSIS OF SAMPLES FROM SITES 397 AND 398 Daniel B. Pearson, The Superior Company, Houston, Texas and Wallace G. Dow, Getty Company, Houston, Texas 1 INTRODUCTION Economic interest in
More informationDetailed Sedimentology and Inorganic Geochemistry of the Dolgeville Formation and Utica Group of the Central Mohawk Valley, NY
Detailed Sedimentology and Inorganic Geochemistry of the Dolgeville Formation and Utica Group of the Central Mohawk Valley, NY Daniel Miserendino Jeffrey T. Pietras Introduction and Purpose Drill cores
More informationUpdate on Horse Hill discovery, UK Weald Basin Update on Nutech well analysis - Further potential oil pay identified
18 March 2015 Alba Mineral Resources plc ( Alba or the Company ) Update on Horse Hill discovery, UK Weald Basin Update on Nutech well analysis - Further potential oil pay identified Alba is pleased to
More informationDrill Cuttings Analysis: How to Determine the Geology of a Formation and Reservoir
Drill Cuttings Analysis: How to Determine the Geology of a Formation and Reservoir Chuck Stringer ASA Manager Southern Region 2015 TECH MKT_2014-BD-REG-1673 1 The one item that has lacked serious consideration
More informationGeology 252, Historical Geology, California State University, Los Angeles - professor: Dr. Alessandro Grippo
LAB # 1 - CLASTIC ROCKS Background: - Mechanical and Chemical Weathering - Production of Clastic Sediment - Classification of Sediment according to size: Gravel, Sand, Silt, Clay - Erosion, Transportation
More informationEarth Materials Unit: Sedimen ntary Rocks and Processes Maybe One Day Text: Chapters Five and Six Lab: Laboratorry Six Name
Earth Materi ials Unit: Sedimentary Rocks and Proces sses Maybe One Day Text: Chapters Fivee and Six Lab: Laboratory Six Name Page 1 Sedimentary Rocks and Processes Purpose: To classify sedimentary rocks
More informationSouth Texas* Paul C. Hackley 1, Kristin Dennen 1, Rachel Gesserman 1, and Jennie L. Ridgley 2
AV Preliminary Investigation of the Thermal Maturity of Pearsall Formation Shales in the Maverick Basin, South Texas* Paul C. Hackley 1, Kristin Dennen 1, Rachel Gesserman 1, and Jennie L. Ridgley 2 Search
More informationOGIP Evaluation of Shale Gas and CBM with Basin Modeling and Gas Isotopes Interpretation*
OGIP Evaluation of Shale Gas and CBM with Basin Modeling and Gas Isotopes Interpretation* Daniel Xia 1,2 and Yongchun Tang 1 Search and Discovery Article #40842 (2011) Posted November 30, 2011 *Adapted
More informationCOMPOSITIONAL TERMS: FELSIC : light colored INTERMEDIATE : medium shades MAFIC : dark colored ULTRAMAFIC : rare (composition of the mantle)
GEOLOGY 306 Laboratory NAME: Instructor: TERRY J. BOROUGHS SECTION: Common Rocks (Chapter 2) For this assignment, you will require: a streak plate, glass plate, magnet, dilute hydrochloric (HCl) acid,
More informationEvaluation of Neocomian Shale source rock In Komombo Basin, Upper Egypt
Evaluation of Neocomian Shale source rock In Komombo Basin, Upper Egypt Abdelhady, A. 1, Darwish, M. 2, El Araby, A. 3 and Hassouba, A. 4 1 DEA Egypt, Cairo, Egypt 2 Geology Department, Faculty of Science,
More informationChert-Shale-Mudstone Chert typs of silica: Microquartz Megaquartz Chalcedonic quartz (From Tucker, 1996)
Chert-Shale-Mudstone Chert is a general term for fine-grained siliceous rock, of chemical, biochemical, biogenetic origin. It is a dense, very hard rock, which splinters with a conchoidal fracture. The
More informationThere are five main methods whereby an unstable isotope can gain stability by losing energy. These are:
10. RADIOACTIVITY LOGGING 10.1 Introduction Radioactivity is used in several different types of logging tool. There are those that measure the natural radiation generated by the formation, such as the
More informationPetroleum System Modelling applied to the evaluation of HC in Place in Unconventional Gas Shale prospects
Petroleum System Modelling applied to the evaluation of HC in Place in Unconventional Gas Shale prospects Domenico Grigo 28 April, 2011 www.eni.it applied to Gas Shale Prospect characterisation Why? In
More informationGEOL 101 Lecture 7. Weathering, Sediments. Rock Cycle. Least Stable. Most Stable. Weathering Ch. 5. Physical. Chemical
GEOL 101 Lecture 7 Weathering, Sediments S. Kite Photo Bear Butte S.P., SD Rock Cycle Weathering Ch. 5 Physical (later) Chemical (now) Bowen s Reaction Series vs. Goldich s Weathering Series for sand-size
More informationCEE 437 Lecture 11 Rock Classification. Thomas Doe
CEE 437 Lecture 11 Rock Classification Thomas Doe Translation of Mineral Properties to Rock Properties Comparison of mineral properties to rock properties Rocks have lower strength, especially tensile
More informationGEOLOGICAL LOG INTERPRETATION TUTORIAL
GEOLOGICAL LOG INTERPRETATION TUTORIAL Text and Figures by Geoff Bohling and John Doveton The following pages will familiarize you with the basics of the geological interpretation of common logs as they
More informationOverview of Selected Shale Plays in New Mexico*
Overview of Selected Shale Plays in New Mexico* Ron Broadhead 1 Search and Discovery Article #10627 (2014)** Posted August 18, 2014 *Adapted from presentation at RMAG luncheon meeting, Denver, Colorado,
More informationVirginia T. McLemore, New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801,
Virginia T. McLemore, New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801, ginger@gis.nmt.edu U2011, Casper, Wy September 20, 2011 Acknowledgments
More informationGuided Notes Rocks & Minerals
Guided Notes Rocks & Minerals is Mineral 1.What is a Mineral Tests 2.Mineral Properties Cycle 3.Rock Rocks 4.Igneous Rocks 5.Sedimentary Rocks 6. Metamorphic Rocks Reference Tables K. Coder 2015 12. What
More informationAlgeo et al. Changes in ocean denitrification during Late Carboniferous glacial-interglacial cycles NGS
Algeo et al. Changes in ocean denitrification during Late Carboniferous glacial-interglacial cycles NGS-27-11-379 Supplementary Methods Crossplots of total organic carbon (TOC) versus total nitrogen (TN)
More informationSediment and sedimentary rocks Sediment
Sediment and sedimentary rocks Sediment From sediments to sedimentary rocks (transportation, deposition, preservation and lithification) Types of sedimentary rocks (clastic, chemical and organic) Sedimentary
More informationThe Niobrara Petroleum System, Rocky Mountain Region. Steve Sonnenberg & James Taylor Colorado School of Mines
The Niobrara Petroleum System, Rocky Mountain Region Steve Sonnenberg & James Taylor Colorado School of Mines The Niobrara-Mancos Oil & Gas Play, Rocky Mountain Region Niobrara and Mancos Production, Rocky
More informationROCK CLASSIFICATION AND IDENTIFICATION
Name: Miramar College Grade: GEOL 101 - Physical Geology Laboratory SEDIMENTARY ROCK CLASSIFICATION AND IDENTIFICATION PRELAB SECTION To be completed before labs starts: I. Introduction & Purpose: The
More informationStructure contours on Bone Spring Formation (Lower Permian), Delaware Basin
Structure contours on Bone Spring Formation (Lower Permian), Delaware Basin By Ronald F. Broadhead and Lewis Gillard New Mexico Bureau of Geology and Mineral Resources, a division of New Mexico Tech, Socorro
More informationSediments and Sedimentary Rocks
Sediments and Sedimentary Rocks (Shaping Earth s Surface, Part 2) Science 330 Summer 2005 What is a sedimentary rock? Products of mechanical and chemical weathering Account for about 5 percent of Earth
More informationFY 2013 Annual Technical Report for NCRDS State Cooperative Program
FY 2013 Annual Technical Report for NCRDS State Cooperative Program SUBSURFACE GAS-SHALE SAMPLES OF THE UPPER DEVONIAN AND LOWER MISSISSIPPIAN WOODFORD SHALE, PERMIAN BASIN, WEST TEXAS AND SOUTHEASTERN
More informationCore Technology for Evaluating the Bakken
Core Technology for Evaluating the Bakken Fundamentals for Reservoir Quality Assessment and Completion Analysis John Kieschnick and Roberto Suarez-Rivera TerraTek 1 Topics Covered Core Technology Changes
More informationReview - Unit 2 - Rocks and Minerals
Review - Unit 2 - Rocks and Minerals Base your answers to questions 1 and 2 on the diagram below, which shows the results of three different physical tests, A, B, and C, that were performed on a mineral.
More informationRock Eval, Total Organic Carbon of the 29 rock samples from Mali. Unfiled Report April
Rock Eval, Total Organic Carbon of the 29 rock samples from Mali Unfiled Report April 26 2011 Dear Sir, We have analyzed your 29 rock samples from Mali. The rock samples were pyrolyzed using our Rock-Eval
More informationM. Elgmati, H. Zhang, M. Zobaa, B. Bai, and F. Oboh-Ikuenobe. June 15 th, 2011
M. Elgmati, H. Zhang, M. Zobaa, B. Bai, and F. Oboh-Ikuenobe June 15 th, 2011 Purposes Palynofacies Analysis Kerogen Type Thermal Maturation Estimated Key Geochemical Parameters Total Organic Carbon 3D
More informationEarth Science 11 Learning Guide Unit 5
Earth Science 11 Learning Guide Unit 5 Name: 5-1 Minerals and mineral identification 1. For each of the following statements put a R in the space if the statement refers to a rock M in the space if the
More informationENGLE COAL FIELD. David E. Tabet
OPEN FILE REPORT 115 SUMMARY OF THE GEOLOGY OF THE ENGLE COAL FIELD by David E. Tabet THE ENGLE COAL FIELD Introduction The Engle coal field (Lee, 1905), named for the small town of Engle along the Santa
More informationSand. Sand is any eroded material (igneous, metamorphic or sedimentary) that has a grain size from 1/16 th to 2 millimeters in size.
Sedimentology 001 What is sedimentology? Sedimentology...encompasses the study of modern sediments such as sand [1], mud (silt) [2] andclay [3] and understanding the processes that deposit them.[4] It
More informationBy Steven Schamel 1. Search and Discovery Article # (2007 Posted September 13, Abstract
AV Utah Shale Gas: A Developing Resource Play* By Steven Schamel 1 Search and Discovery Article #110067 (2007 Posted September 13, 2008 *Prepared for presentation at AAPG Annual Convention, San Antonio,
More informationLaboratory 5 Sedimentary and Metamorphic Rocks a.
Laboratory 5 Sedimentary and Metamorphic Rocks a. LAB 5 provides samples of all three principal groupings of rocks including: 1) Igneous (plutonic and extrusive felsic, intermediate, and mafic varieties)
More information1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite.
1. Base your answer to the following question on The diagram below represents a part of the crystal structure of the mineral kaolinite. An arrangement of atoms such as the one shown in the diagram determines
More informationMODULE PREREQUISITES FOR HYDROCARBON ACCUMULATION
MODULE 1 1.0 PREREQUISITES FOR HYDROCARBON ACCUMULATION The accumulation of hydrocarbons and formation of oil or gas deposit involve certain prerequisites. These are the following: 1. Source Rock 2. Reservoir
More information1. Gravel-size 2. Sand-size 3. Silt-size 4. Clay-size 5. Microcrystalline 6. Macrocrystalline
Name: GEOL 101 - Physical Geology Lab Grade: SEDIMENTARY & METAMORPHIC ROCK CLASSIFICATION and IDENTIFICATION SEDIMENTARY PRE-ID SECTION To be completed before observing hand samples: I. Introduction &
More informationName: Grade: GEOL Physical Geology Laboratory Sedimentaryand Metamorphic Rocks Lab #6
Name: GEOL 101 - Physical Geology Laboratory Sedimentaryand Metamorphic Rocks Lab #6 Grade: PRELAB SECTION To be completed before labs starts: I. Introduction & Purpose: The purpose of this laboratory
More informationSediment. Weathering: mechanical and chemical decomposition and disintegration of rock and minerals at the surface
Sediment Some basic terminology Weathering: mechanical and chemical decomposition and disintegration of rock and minerals at the surface Erosion: removal of weathered rock and minerals from one place to
More informationNorth GOM Petroleum Systems: Modeling the Burial and Thermal History, Organic Maturation, and Hydrocarbon Generation and Expulsion
North GOM Petroleum Systems: Modeling the Burial and Thermal History, Organic Maturation, and Hydrocarbon Generation and Expulsion Roger J. Barnaby 2006 GCAGS MEETING Previous studies of northern GOM crude
More informationMeasurement of the organic saturation and organic porosity in. shale
Measurement of the organic saturation and organic porosity in shale Qian Sang a,b, Shaojie Zhang a, Yajun Li a, Mingzhe Dong a,b Steven Bryant b a College of Petroleum Engineering, China University of
More informationRocks. 3.1 The Rock Cycle. 3.1 The Rock Cycle. 3.1 The Rock Cycle. The Rock Cycle. I. Rocks
Rocks Tarbuck Lutgens 3.1 The Rock Cycle 3.1 The Rock Cycle I. Rocks Rocks are any solid mass of mineral or mineral-like matter occurring naturally as part of our planet. Types of Rocks 1. Igneous rock
More informationSEDIMENTARY ROCKS FROM THE CONTINENTAL SHELF AND SLOPE OFF THE CENTRAL COAST OF OREGON. By Neil J. Maloney and John V. Byrne
SEDMENTARY ROCKS FROM THE CONTNENTAL SHELF AND SLOPE OFF THE CENTRAL COAST OF OREGON By Neil J. Maloney and John V. Byrne Reprinted from: The ORE BN, vol. 26, no. 5, May 1964 Oregon Department of Geology
More informationMinerals and Rocks Chapter 20
Minerals and Rocks Chapter 20 Emily and Megan Earth System Science Interconnected Rocks and minerals Interior processes Erosion and deposition Water and air Elements of Earth by weight Made of atoms Earth
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 3 Rocks 3.1 The Rock Cycle Rocks Rocks are any solid mass of mineral or mineral-like matter occurring naturally as part of our planet. Types of Rocks
More informationOil Impregnated Sandstone STUDY NEAR BRUIN POINT. AND RANGE CREEK - Sunnyside. Quadrangle. June D. Craig Mann & Sam Quigley
Oil Impregnated Sandstone STUDY NEAR BRUIN POINT AND RANGE CREEK - Sunnyside Quadrangle June 1972 by D. Craig Mann & Sam Quigley INTRODUCTION An investigation into the oil sandstones in the Book Cliffs
More informationIsothermal and Nonisothermal Kinetic Analyses of Mahogany Oil Shale with TGA
Isothermal and Nonisothermal Kinetic Analyses of Mahogany Oil Shale with TGA Pankaj Tiwari, Kyeongseok Oh and Milind Deo Chemical Engineering Dept, University of Utah 1 Table of contents Introduction Background
More informationLaboratory 5. Sedimentary Rocks
Laboratory 5. Sedimentary Rocks The two primary types of sediment are chemical and detrital. Sediment becomes lithified into sedimentary rocks by cementation and compaction. Chemical sedimentconsists of
More informationSedimentary Rocks. Weathering. Mechanical & Chemical Weathering. Sediments. Lithification. Deposition. Transport. Erosion.
Lithification Sedimentary Rocks Sediments Deposition Transport Erosion Weathering Weathering The sediments that make up sedimentary rocks are produced by: Mechanical & Chemical Weathering Mechanical Weathering
More informationDiscovering STEM Program
Discovering STEM Program Identifying Rock Types Activity (upper elementary) Rock Types Rock Sample Numbers I=igneous S=sedimentary M=metamorphic 1 2 3 4 5 6 7 8 9 10 11 12 Using above properties determine
More informationEmily and Megan. Earth System Science. Elements of Earth by weight. Crust Elements, by weight. Minerals. Made of atoms Earth is mostly iron, by weight
Emily and Megan Chapter 20 MINERALS AND ROCKS Earth System Science Interconnected Rocks and minerals Interior processes Erosion and deposition Water and air Elements of Earth by weight Made of atoms Earth
More information4/4. K What I know about Sedimentary Rocks. W What I want to find out about Sedimentary Rocks Sunday, April 7, 13
Do Now (2 minutes) 4/4 K What I know about Sedimentary Rocks W What I want to find out about Sedimentary Rocks 1. 2. 3. 1. 2. 3. The Rock Cycle What is the rock cycle and how do rocks interrelate? Rock
More informationCalculating Total Organic Carbon (TOC) using the Passey Method
Calculating Total Organic Carbon (TOC) using the Passey Method Chris Gent Overview 1. Passey method 2. Importance of TOC and maturity data. 3. Case Study: The Weald, UK. 1. The Passey Method A Practical
More informationCharacterization and comparison of mine wastes from legacy mines in NM
Characterization and comparison of mine wastes from legacy mines in NM Presentation by: John Asafo-akowuah May 23, 2017 Overview Purpose Study Area Methodology Results Preliminary Conclusions Future Work
More informationSedimentary Rocks. Rocks made of bits & pieces of other rocks.
Sedimentary Rocks Rocks made of bits & pieces of other rocks. Sedimentary Rocks Igneous rocks are the most common rocks on Earth, but because most of them exist below the surface you might not have seen
More information15. THE NEUTRON LOG 15.1 Introduction
15. THE NEUTRON LOG 15.1 Introduction The neutron log is sensitive mainly to the amount of hydrogen atoms in a formation. Its main use is in the determination of the porosity of a formation. The tool operates
More informationo - 399' ' ' ' ' T. D.
Ii I I' I: VDMRWellNo W-1142 Operator: J W Miloncus Farm: Browning Wynn Well No. : 1 Location: Lee County 3300' N of 36 042'30" 1800' E of 83005' approx Elevation: 1975' (reported altimeter elevation)
More informationChallenge of Mae Sot Oil Shale Exploration in Thailand (In the First Phase, 2008) Apichart Jeennagol Apiradee Suwannathong
Challenge of Mae Sot Oil Shale Exploration in Thailand (In the First Phase, 2008) by Apichart Jeennagol Apiradee Suwannathong The 28 th Oil Shale Symposium October 15, 2008 Colorado School of Mines, Golden,
More informationf/.j. / A ' i i i y y / /*/ /V / / /'/V'/ / / D J ^ OSLO STAVANGER WELL NAME r \ TRAENAPANKEN 6609/7-1 NEPIUNO NORDRAU / y 20/ /20 23/ 1.
D J ^ OSLO STAVANGER WELL NAME 6609/7 AENAPANKEN AREA Drilling Mud Properties Record OPERATOR PPCON NEPIUNO NORDRAU RIG. MUD SYSTEM GEL/SEAWATER GEL/DRISPAC ENGINEERS FOLKVDRD/TORGERSENAAURITZEN Day No
More informationGeochemical Evaluation of (Late Jurassic) Naokelekan Formation /Zagros Fold Belt, North Iraq
Proceeding of 3 rd scientific conference of the College Al-Ahmed Proceeding of 3 rd of Science, University of Baghdad. scientific conference, 2009, PP. 1769-1775 24 to 26 March 2009. Geochemical Evaluation
More informationCEE 437 Lecture 10 Rock Classification. Thomas Doe
CEE 437 Lecture 10 Rock Classification Thomas Doe Igneous Origins Intrusive Batholithic or plutonic: phaneritic Dikes or sills that chill rapidly: aphanitic Extrusive deposition as melt (lava) pyroclastic
More informationAPPLICATIONS OF PETROLEUM SYSTEMS MODELING IN CCUS
APPLICATIONS OF PETROLEUM SYSTEMS MODELING IN CCUS 2017 CO 2 for EOR as CCUS Conference: Houston, TX GRAGG, Evan 1, VAN WIJK, Jolante 1 and BALCH, Robert 2 (1) Department of Earth and Environmental Science,
More informationOil Shale Project in Thailand
Oil Shale Project in Thailand Progress of Oil Shale Exploration in Thailand (Phase 2) The cooperation of Thai agencies between Department of Mineral Fuels (DMF) and Electricity Generating Authority of
More informationKinetic modelling of kerogen cracking during oil shale process : influence of organic matter source F. Behar and P. Allix
Kinetic modelling of kerogen cracking during oil shale process : influence of organic matter source F. Behar and P. Allix 1 General outline! I Introduction! II Kerogen characterization Definition of the
More informationAn outcrop analogue for the Williston Basin Bakken hybrid play, the Sappington Formation in southwest Montana:
An outcrop analogue for the Williston Basin Bakken hybrid play, the Sappington Formation in southwest Montana: Facies, stratigraphic architecture, and controls on porosity distribution Michael Hofmann
More informationUNIT 4 SEDIMENTARY ROCKS
UNIT 4 SEDIMENTARY ROCKS WHAT ARE SEDIMENTS Sediments are loose Earth materials (unconsolidated materials) such as sand which are transported by the action of water, wind, glacial ice and gravity. These
More informationLEGEND ODOT CLASS. A-4b. A-6a. A-6b TOTAL VISUAL WEATHERED SANDSTONE VISUAL BORING LOCATION - PLAN VIEW
PROJECT THE PROJECT CONSISTS IN PART OF ACING TWO STRUCTURES, EASTBOUND AND WESTBOUND STRUCTURES, RESPECTIVELY FOR THE PROPOSED SR OVER BLUE ROAD (CR 9). THE TWO STRUCTURES AS ANNED, ARE SINGLE-SPAN STRUCTURES
More informationGeology 229 Engineering Geology. Lecture 6. Basic Rock Classification and Engineering Considerations (West, Chs. 2, 3, 4, 5)
Geology 229 Engineering Geology Lecture 6 Basic Rock Classification and Engineering Considerations (West, Chs. 2, 3, 4, 5) Outline of this Lecture 1. Rock types and rock cycle 2. Geological and engineering
More informationAs compaction and cementation of these sediments eventually occur, which area will become siltstone? A) A B) B C) C D) D
1. A student obtains a cup of quartz sand from a beach. A saltwater solution is poured into the sand and allowed to evaporate. The mineral residue from the saltwater solution cements the sand grains together,
More informationGeology of the RC Westfork Cemetery Ridge Solution Collapse Breccia, Viburnum Trend, Southeast Missouri. By Thomas Schott
Geology of the RC Westfork Cemetery Ridge Solution Collapse Breccia, Viburnum Trend, Southeast Missouri By Thomas Schott Introduction Viburnum Trend Pb-Zn mineralization is blind Historically poor results
More informationFusselman/Devonian Study. of the Midland Basin, Texas
Fusselman/Devonian Study of the Midland Basin, Texas Fusselman-Devonian Study of the Midland Basin, Texas Overview The Fusselman-Devonian study of the Midland Basin is designed to enhance both exploration
More informationGEOL.3250 Geology for Engineers Sedimentary & Metamorphic Rocks
GEOL.3250 Geology for Engineers Sedimentary & Metamorphic Rocks Name I. Introduction The bulk of the earth's crust is composed of relatively few minerals. These can be mixed together, however, to give
More informationWhich sample best shows the physical properties normally associated with regional metamorphism? (1) A (3) C (2) B (4) D
1 Compared to felsic igneous rocks, mafic igneous rocks contain greater amounts of (1) white quartz (3) pink feldspar (2) aluminum (4) iron 2 The diagram below shows how a sample of the mineral mica breaks
More informationGeology for Engineers Rocks
89.325 Geology for Engineers Rocks Name I. Introduction The bulk of the earth's crust is composed of relatively few minerals. These can be mixed together, however, to give an endless variety of rocks -
More informationLithology Evaluation of Bazhenov Formation Reservoir using Seismic and Well Log Analysis
Lithology Evaluation of Bazhenov Formation Reservoir using Seismic and Well Log Analysis N Y Lomakina Petroleum Learning Centre Tomsk Polytechnic University Tomsk, Russia Abstract Bazhenov formation is
More informationWhich rock is shown? A) slate B) dunite C) gneiss D) quartzite
1. Which metamorphic rock will have visible mica crystals and a foliated texture? A) marble B) quartzite C) schist D) slate 2. The recrystallization of unmelted material under high temperature and pressure
More information5. The table below indicates the presence of various minerals in different rock samples.
1. Which mineral is composed of Calcium and Fluorine? A) Amphiboles B) Calcite C) Hematite D) Fluorite 2. The photograph below shows a broken piece of the mineral calcite. The calcite breaks in smooth,
More informationThermal Maturity of the Marcellus Shale and the Line of Death : NE Pennsylvania
Thermal Maturity of the Marcellus Shale and the Line of Death : NE Pennsylvania Conducted by Ethan Shula Department of Science & Mathematics Cedarville University, Cedarville, Ohio eshula@cedarville.edu
More information