Asbestos fibres release from serpentinites during quarry operations: case studies from eastern ligurian ophiolites

Size: px
Start display at page:

Download "Asbestos fibres release from serpentinites during quarry operations: case studies from eastern ligurian ophiolites"

Transcription

1 Marescotti P., Gaggero L., Isola E., Malatesta C., Solimano M. DIPTERIS Università di Genova Asbestos fibres release from serpentinites during quarry operations: case studies from eastern ligurian ophiolites Asbesto Risk and Management Roma, 4-6 Dicembre 2006

2 Scale 1:5000 C Year I.R. (limit = 0.1) Method Classification Mechanical scratching Not dangerous Mechanical scratching Not dangerous Mechanical scratching Not dangerous Mechanical scratching Not dangerous Grinding machine Not dangerous Grinding machine Not dangerous Grinding machine Not dangerous Grinding machine Not dangerous Grinding machine Not dangerous Grinding machine Not dangerous Grinding machine Not dangerous 2006 <0.001 Grinding machine Not dangerous 2006 <0.001 Grinding machine Not dangerous 2006 <0.001 Grinding machine Not dangerous B A

3 Scale 1:5000 C B A

4 C B A

5 Field geological and minero-petrographical analyses (following the UNI EN ISO Rocks identification and classification, modified and adapted for the specific case of asbestos-bearing rocks) Complete census of fibres and fibre sheaves occurrences at the outcrop scale Mapping of the quarry fronts and definition of the sampling strategy Mineralogical and petrographical qualitative and quantitative analyses Stereo Microscope (representativity of the sample, selection of sample for further investigations, detection of fibres, estimation of percentage composition) Polarized light microscopy (textural analyses, minerals identification, evaluation of percentage composition by visual estimation and/or point counting) XRPD (minerals identification and quantitative analyses)

6 massive Field geological and minero-petrographical analyses (Quarry A) serpentinites fractured serpentinites fractured serpentinites Scale 1:5000 cataclastic serpentinites

7 mineralogy of massive serpentinites major constituents (in order of decreasing abundance) Lizardite (60-70%) Chrysotile(25-35%) Magnetite( 5%) minor constituents (in order of decreasing abundance) Chlorite Calcite Dolomite Talc

8 massive serpentinites 5 mm mesh textures

9 massive serpentinites 5 mm bastite

10 massive serpentinites 0.5 mm 5 mm ribbon textures

11 mineralogy of fractured and cataclastic serpentinites major constituents (in order of decreasing abundance) Lizardite (50-60%) Chrysotile(35-45%) Magnetite( 5%) minor constituents (in order of decreasing abundance) Chlorite Calcite and Dolomite Tremolite Talc

12 a) serrate chrysotile veins with rigid fibres perpendicular to the vein walls 0.1 mm 5 mm 10-15% of the analyzed veins filling minerals: chrysotile fibre type: easily detachable rigid fibres fibres lenght: mm fibres diameter: mm

13 a) composite chrysotile veins with chaotic growth of soft fibres 0.1 mm 0.5 mm % of the analyzed veins filling minerals: chrysotile ± chlorite ± calcite ± dolomite ± talc fibre type: easily detachable bundles and sheaves of soft fibres fibres lenght: mm fibres diameter: mm

14 a) slip chrysotile veins with parallel aggregates of rigid fibres 1 cm 1 mm 0.1 mm % of the analyzed veins filling minerals: chrysotile ± chlorite fibre type: easily detachable rigid fibres fibres lenght: 5-50 mm fibres diameter: mm

15 Serpentinites Volume in outcrop Mineralogy (major costituents) Asbestos type Fibres lenght (mm) Massive 20-25% lizardite, chrysotile, magnetite chrysotile mass.tex veins Fractured 70-75% lizardite, chrysotile, magnetite, chlorite, talc, calcite Cataclastic 1-5% lizardite, chrysotile, tremolite, magnetite, chlorite, talc, calcite chrysotile chrysotile, tremolite mass.tex veins mass.tex veins Asbestos concentration (XRPD, SEM, PLOM) (mg/kg) (mg/kg) (mg/kg)

16 Free fibres evidences in the quarry fronts

17 Free fibres evidences in the quarry fronts

18 Free fibres evidences in soils and uncosolidated sediments

19 Mineralogy and petrography of quarry soils and uncosolidated sediments Agravel Asand Asoil Bsoil Csoil wt %

20 (355 µm <ø< 1mm): stereo microscope 0.5 mm soil quarry A soil quarry B 1 mm 1 mm detrites quarry A floor 0.5 mm detrites quarry A floor

21 (355 µm <ø< 1mm): polarized light microscopy 0.3 mm 1 mm 0.5 mm 0.5 mm

22 (355 µm <ø< 1mm): polarized light microscopy 0.3 mm Massive Friable Other 60 1 mm 50 wt% mm AF1 AF2 AF3 AS1 AS2 BS1 BS2 BS3 CS1 CS2 0.5 mm

23 <53 µm : water suspension (plane polarized light microscopy) PPL 0.01 mm PPL 0.05 mm 0.01 mm

24 <53 µm : water suspension (plane polarized light microscopy) mean value of 50 fields (field area = 2mm 2 ) Af As Bs Cs 20 PPL n of fibres mm PPL mm 0.01 mm

25 <53 µm : water suspension (plane polarized light microscopy) 10 PPL n of fibres sample/n fibres standard soil mm PPL Af As Bs Cs 0.05 mm 0.01 mm

26

27 Estimation of the mean asbestos content of the quarry Determination of the release index Analytical control on the atmospheric aerosol particles Structural and textural characterization of the outcropping rocks Distinction between rocks containing non-releasable (i.e massive) and easily releasable (i.e. friable) asbestos fibres. Mapping of a) occurrences of asbestos free fibres and fibrous bundles; b) occurrences of friable asbestos bearing masses and veins Evaluation of the natural level of asbestos contamination, not only in air, but also in soils and sediments

Thin and short chrysotile fibres: an additional hazard?

Thin and short chrysotile fibres: an additional hazard? Thin and short chrysotile fibres: an additional hazard? Requested by R.S.A Srl Balangero to Interdepartmental Centre G. Scansetti for Studies on Asbestos and Other Toxic Particulates University of Torino

More information

Rock & Minerals Regents Review

Rock & Minerals Regents Review Name Rock & Minerals Regents Review Base your answers to questions 1 through 3 on the diagram below, which represents a part of the rock cycle. The igneous rock granite, and the characteristics of sedimentary

More information

I.S : What s in it and the role of the Geologist

I.S : What s in it and the role of the Geologist Institute of Geologists of Ireland Pyrite Course I.S. 398-1: What s in it and the role of the Geologist Michael L.J. Maher 4 December, 2013 Responsibilities of Geologist You re only the messenger! Classification

More information

Naturally Occurring Asbestos:

Naturally Occurring Asbestos: RJ LeeGroup, Inc. Naturally Occurring Asbestos: A Recurring Public Policy Challenge R. J. Lee, B. R. Strohmeier, K. L. Bunker, and D. R. Van Orden RJ Lee Group, Inc. 350 Hochberg Road Monroeville, PA 15146

More information

Listvenites as targets for Au-Hg mineralization in Central Iran ophiolites

Listvenites as targets for Au-Hg mineralization in Central Iran ophiolites Listvenites as targets for Au-Hg mineralization in Central Iran ophiolites Fatemeh Mohammadi*,Moosa Noghreian**,Mohammad Ali Mackizadeh**,Babak Vahabimogha *Islamic Azad university of khorasgan,esfahan,iran.

More information

Petrography and mineralogy of ultamafic rocks in Nain Ophiolite (Central Iran)

Petrography and mineralogy of ultamafic rocks in Nain Ophiolite (Central Iran) Petrography and mineralogy of ultamafic rocks in Nain Ophiolite (Central Iran) Mohammad Foudazi 1 Mohammad Hashem Emami 2 Soleiman Alai Mahabadi 2 1-IslamicAzad University,Science and Research Branch 2-Geological

More information

Proposed Testing and Research Approach for Pyrrhotite-Induced Concrete Deterioration

Proposed Testing and Research Approach for Pyrrhotite-Induced Concrete Deterioration 1 Proposed Testing and Research Approach for Pyrrhotite-Induced Concrete Deterioration Mr. Christopher M. Moore, Mr. Cody M. Strack, Dr. Robert D. Moser, Dr. Gordon W. McMahon, Engineer Research and Development

More information

Solapur University, Solapur. Syllabus for B.Sc. II- Geochemistry - (IDS) Semester System - CGPA To be implemented from Academic Year

Solapur University, Solapur. Syllabus for B.Sc. II- Geochemistry - (IDS) Semester System - CGPA To be implemented from Academic Year Solapur University, Solapur Syllabus for B.Sc. II- Geochemistry - (IDS) Semester System - CGPA To be implemented from Academic Year- 2015-16 Course Structure Total Credit 16 - (Theory (4 x 3) = 12+Practical

More information

SAMREC 2009 Table 1, Section 5.5 Treatment / Processing

SAMREC 2009 Table 1, Section 5.5 Treatment / Processing Volume 58 ~ Number TWO ~ JUNE 2015 SAMREC 2009 Table 1, Section 5.5 Treatment / Processing ASSESSMENT CRITERION: T 5.5 Treatment / Processing EXPLORATION RESULTS (A) (i) Describe any obvious processing

More information

RAMAN SPECTROSCOPY OF ASBESTOS - POLYMORPHS OF SERPENTINE

RAMAN SPECTROSCOPY OF ASBESTOS - POLYMORPHS OF SERPENTINE UNIVERSITÀ DEGLI STUDI DI PARMA Dipartimento di Fisica e Scienze della Terra Parma -Italy UNIVERSITÉ DE LA NOUVELLE CALEDONIE Laboratoire PPME RAMAN SPECTROSCOPY OF ASBESTOS - POLYMORPHS OF SERPENTINE

More information

This document is a preview generated by EVS

This document is a preview generated by EVS INTERNATIONAL STANDARD ISO 22262-1 First edition 2012-07-01 Air quality Bulk materials Part 1: Sampling and qualitative determination of asbestos in commercial bulk materials Qualité de l air Matériaux

More information

Detrick, R., Honnorez, J., Bryan, W. B., Juteau, T., et al., 1990 Proceedings of the Ocean Drilling Program, Scientific Results, Vol.

Detrick, R., Honnorez, J., Bryan, W. B., Juteau, T., et al., 1990 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. Detrick, R., Honnorez, J., Bryan, W. B., Juteau, T., et al., 1990 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 106/109. ROCK MAGNETIC PROPERTIES AND OPAQUE MINERALOGY OF SELECTED

More information

Serpentine minerals from veins in serpentinite rocks

Serpentine minerals from veins in serpentinite rocks MNERALOGCAL MAGAZNE, MARCH 97 9, VOL. 43, PP. 35-4o Serpentine minerals from veins in serpentinite rocks stituto di Mineralogia e Petrografia dell'universit~t di Bologna, taly SUMMARY. Crystal-chemical

More information

Geology 229 Engineering Geology. Lecture 7. Rocks and Concrete as Engineering Material (West, Ch. 6)

Geology 229 Engineering Geology. Lecture 7. Rocks and Concrete as Engineering Material (West, Ch. 6) Geology 229 Engineering Geology Lecture 7 Rocks and Concrete as Engineering Material (West, Ch. 6) Outline of this Lecture 1. Rock mass properties Weakness planes control rock mass strength; Rock textures;

More information

Serpentine Mine, Cyprus, 2007

Serpentine Mine, Cyprus, 2007 Serpentine Mine, Cyprus, 2007 What is an ophiolite? Simply: Ophiolites are pieces of oceanic crust found on land The international ophiolite conference restricted the term ophiolite to only include the

More information

Name: Minerals and more minerals

Name: Minerals and more minerals 1. The diagram below shows how a sample of the mineral mica breaks when hit with a rock hammer. 6. The diagrams below show the crystal shapes of two minerals. This mineral breaks in smooth, flat surfaces

More information

GEOL Lab 9 (Carbonate Sedimentary Rocks in Hand Sample and Thin Section)

GEOL Lab 9 (Carbonate Sedimentary Rocks in Hand Sample and Thin Section) GEOL 333 - Lab 9 (Carbonate Sedimentary Rocks in Hand Sample and Thin Section) Sedimentary Rock Classification - As we learned last week, sedimentary rock, which forms by accumulation and lithification

More information

Metamorphism (means changed form

Metamorphism (means changed form Metamorphism (means changed form) is recrystallization without melting of a previously existing rock at depth in response to a change in the environment of temperature, pressure, and fluids. Common minerals

More information

NOTE FIBROUS CLAY MINERAL COLLAPSE PRODUCED BY BEAM DAMAGE OF CARBON-COATED SAMPLES DURING SCANNING ELECTRON MICROSCOPY

NOTE FIBROUS CLAY MINERAL COLLAPSE PRODUCED BY BEAM DAMAGE OF CARBON-COATED SAMPLES DURING SCANNING ELECTRON MICROSCOPY Clay Minerals (1991) 26, 141-145 NOTE FIBROUS CLAY MINERAL COLLAPSE PRODUCED BY BEAM DAMAGE OF CARBON-COATED SAMPLES DURING SCANNING ELECTRON MICROSCOPY Authigenic fibrous clays often occur in the pore

More information

Geogenic versus Anthropogenic Metals and Metalloids

Geogenic versus Anthropogenic Metals and Metalloids Geogenic versus Anthropogenic Metals and Metalloids Geochemical methods for evaluating whether metals and metalloids are from geogenic versus anthropogenic sources 1 Definitions Geogenic from natural geological

More information

NOA ASSESSMENT HARRIS QUARRY MENDOCINO COUNTY, CALIFORNIA TABLE OF CONTENTS

NOA ASSESSMENT HARRIS QUARRY MENDOCINO COUNTY, CALIFORNIA TABLE OF CONTENTS NOA ASSESSMENT HARRIS QUARRY MENDOCINO COUNTY, CALIFORNIA TABLE OF CONTENTS Introduction... 1 Scope of Services... 1 Project Location and Description... 1 Geologic Setting... 1 Regional Geology... 1 Site

More information

muscovite PART 4 SHEET SILICATES

muscovite PART 4 SHEET SILICATES muscovite PART 4 SHEET SILICATES SHEET SILICATES = PHYLLOSILICATES Phyllon = leaf Large group of mineral including many common minerals: muscovite, biotite, serpentine, chlorite, talc, clay minerals Structure:

More information

Introduction to Prospecting. Session Three Minerals

Introduction to Prospecting. Session Three Minerals Introduction to Prospecting Session Three Minerals Mineral: Solid inorganic substance of natural occurrence with a specific elemental composition and crystal structure. Rock: An aggregate of minerals.

More information

Earth Science 232 Petrography

Earth Science 232 Petrography Earth Science 232 Petrography Course notes by Shaun Frape and Alec Blyth Winter 2002 1 Petrology - Introduction Some Definitions Petra Greek for rock Logos Greek for disclosure or explanation Petrology

More information

Fro. 2. Fibrous brucite in vein of chrysotile asbestos, Asbestos, Quebec. Pr,ern I. Frc. 1. Photograph of fibrous brucite from Asbestos, Quebec.

Fro. 2. Fibrous brucite in vein of chrysotile asbestos, Asbestos, Quebec. Pr,ern I. Frc. 1. Photograph of fibrous brucite from Asbestos, Quebec. Pr,ern I Frc. 1. Photograph of fibrous brucite from Asbestos, Quebec. sbe stos Fro. 2. Fibrous brucite in vein of chrysotile asbestos, Asbestos, Quebec. Frc. 3. Sketch of photograph in Fig. 2, to show

More information

Aggregates for Concrete

Aggregates for Concrete Fine Aggregate Sand and/or crushed stone < 5 mm (0.2 in.) F.A. content usually 35% to 45% by mass or volume of total aggregate Coarse Aggregate Gravel and crushed stone 5 mm (0.2 in.) typically between

More information

Thickness, Compositional and Textural Variability, and Genesis of El-Lajjun Oil Shale, Central Jordan

Thickness, Compositional and Textural Variability, and Genesis of El-Lajjun Oil Shale, Central Jordan Thickness, Compositional and Textural Variability, and Genesis of El-Lajjun Oil Shale, Central Jordan H Alnawafleh 1, D Large 2 & B Spiro 3 1 Department of Mining Engineering, Al-Hussein Bin Talal University,

More information

Chrysotile and polygonal serpentine from the Balangero serpentinite

Chrysotile and polygonal serpentine from the Balangero serpentinite MINERALOGICAL MAGAZINE, JUNE 1986, VOL. 50, PP. 301-5 Chrysotile and polygonal serpentine from the Balangero serpentinite MARCELLO MELLINI C.N.R., C.S. Geologia Strutturale e Dinamica dell' Appennino,

More information

CONCRETE IN THE MIDDLE EAST

CONCRETE IN THE MIDDLE EAST CONCRETE IN THE MIDDLE EAST ALKALI REACTIVITY IN CONCRETE STRUCTURES Presented by : Eng. ELIE J. SFEIR INTRODUCTION What is the Alkali-Reactivity? The alkali reaction is a chemical reaction between some

More information

9. The table below shows some properties of four different minerals. Rocks and Minerals A B1

9. The table below shows some properties of four different minerals. Rocks and Minerals A B1 Rocks and Minerals A B1 1. Which element is most abundant in Earth s crust? (1) nitrogen (3) oxygen (2) hydrogen (4) silicon 2. Which group of elements is listed in increasing order based on the percent

More information

Minerals Please do not write on this test packet.

Minerals Please do not write on this test packet. Please do not write on this test packet. 1. The diagram below shows the index minerals of Mohs hardness scale compared with the hardness of some common objects. 2. Base your answer to the following question

More information

A Closer Look At Hydrothermal Alteration and Fluid-Rock Interaction Using Scanning Electron Microscopy

A Closer Look At Hydrothermal Alteration and Fluid-Rock Interaction Using Scanning Electron Microscopy Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 A Closer Look At Hydrothermal Alteration and Fluid-Rock Interaction Using Scanning Electron Microscopy Bridget Y. Lynne

More information

Earth Science Minerals. Moh s Scale of Hardness In which New York State landscape region was most of the garnet mined?

Earth Science Minerals. Moh s Scale of Hardness In which New York State landscape region was most of the garnet mined? Name: ate: 1. Which mineral is white or colorless, has a hardness of 2.5, and splits with cubic cleavage? A. calcite. halite C. pyrite. mica 2. ase your answer(s) to the following question(s) on the map

More information

PETROGRAPHIC MINERALOGICAL ANALYSIS OF AGGREGATES FROM DEVOLL HYDROPOWER PROJECT

PETROGRAPHIC MINERALOGICAL ANALYSIS OF AGGREGATES FROM DEVOLL HYDROPOWER PROJECT PETROGRAPHIC MINERALOGICAL ANALYSIS OF AGGREGATES FROM DEVOLL HYDROPOWER PROJECT Rezarta QEMALLAJ 1,dr. ing. Alma GOLGOTA 1 Authors Affiliations: Prof.Dr. Marie Koçi 1 ( KIBE1 Laborator, Durres, Albania)

More information

Lab 6: Metamorphic Rocks

Lab 6: Metamorphic Rocks Introduction The Earth s crust is in a constant state of change. For example, plutonic igneous rocks are exposed at the surface through uplift and erosion. Many minerals within igneous rocks are unstable

More information

WELCOME TO GEOLOGY 333

WELCOME TO GEOLOGY 333 WELCOME TO GEOLOGY 333 Earth Materials and the Environment Lab Instructor: Mike Delucia Office Hours: 11 AM-Noon Wed. and 2-3 PM Th. in 70 CAB Lab Overview Lab Overview: Course Content Lab Policies Introduction

More information

Characterization of Montana Grow Product David Mogk January 16, 2014

Characterization of Montana Grow Product David Mogk January 16, 2014 Characterization of Montana Grow Product David Mogk January 16, 2014 Samples of the raw material that is used in the production of Montana Grow products were characterized using X- ray Powder Diffraction

More information

Mineralogical and technological investigation of pottery and raw materials for ceramic production. Tel el Farcha, Nile Delta. Egypt.

Mineralogical and technological investigation of pottery and raw materials for ceramic production. Tel el Farcha, Nile Delta. Egypt. Maciej Pawlikowski* Mineralogical and technological investigation of pottery and raw materials for ceramic production. Tel el Farcha, Nile Delta. Egypt. */Cath. Mineralogy, Petrography and Geochemistry

More information

Chapter 3 Sedimentation of clay minerals

Chapter 3 Sedimentation of clay minerals Chapter 3 Sedimentation of clay minerals 3.1 Clay sedimentation on land 3.2 From land to sea 3.3 Clay sedimentation in the sea 1 3.1 Clay sedimentation on land Deserts Glaciers Rivers Lacustrine 2 University

More information

CHARACTERIZATION OF NATURAL MATERIALS CONTAINING N.O.A. (NATURALLY OCCURRING ASBESTOS): THE PROBLEM OF QUANTIFICATION

CHARACTERIZATION OF NATURAL MATERIALS CONTAINING N.O.A. (NATURALLY OCCURRING ASBESTOS): THE PROBLEM OF QUANTIFICATION CHARACTERIZATION OF NATURAL MATERIALS CONTAINING N.O.A. (NATURALLY OCCURRING ASBESTOS): THE PROBLEM OF QUANTIFICATION Oliviero Baietto 1, Francesco Amodeo 1, Ilaria Giorgis 1, Martina Vitaliti 1 1 Politecnico

More information

Name: Period: Date: Sedimentary Rock Lab (Formation, Properties, and Ancient Depositional Environments)

Name: Period: Date: Sedimentary Rock Lab (Formation, Properties, and Ancient Depositional Environments) Name: Period: Date: Sedimentary Rock Lab (Formation, Properties, and Ancient Depositional Environments) BIG IDEA: Earth s immense history is recorded in the rocks. Sedimentary rocks tell us about ancient

More information

COMPLEMENTARY METHODS FOR CHARACTERISING SLICK ROCK AEOLIAN SANDSTONE

COMPLEMENTARY METHODS FOR CHARACTERISING SLICK ROCK AEOLIAN SANDSTONE COMPLEMENTARY METHODS FOR CHARACTERISING SLICK ROCK AEOLIAN SANDSTONE S. Baraka-Lokmane, I. Main, S. Elphick, B. Ngwenya Department of Geology & Geophysics, University of Edinburgh, UK INTRODUCTION The

More information

A Regional Diagenetic and Petrophysical Model for the Montney Formation, Western Canada Sedimentary Basin*

A Regional Diagenetic and Petrophysical Model for the Montney Formation, Western Canada Sedimentary Basin* A Regional Diagenetic and Petrophysical Model for the Montney Formation, Western Canada Sedimentary Basin* Noga Vaisblat 1, Nicholas B. Harris 1, Vincent Crombez 2, Tristan Euzen 3, Marta Gasparrini 2,

More information

GSA Data Repository: Three styles of diamond resorption in a single kimberlite

GSA Data Repository: Three styles of diamond resorption in a single kimberlite GSA Data Repository 2017286 Fedortchouk et al., 2017, Three styles of diamond resorption in a single kimberlite: Effects of volcanic degassing and assimilation: Geology, doi:10.1130/g39066.1. 1 2 3 4 5

More information

Factors Contributing to High Gamma-Ray Levels in Early Miocene Bhuban and Boka Bil Sandstone Reservoirs of Titas-15 Well

Factors Contributing to High Gamma-Ray Levels in Early Miocene Bhuban and Boka Bil Sandstone Reservoirs of Titas-15 Well Dhaka Univ. J. Sci. 59(2): 209-216, 2011 (July) Facrs Contributing High Gamma-Ray Levels in Early Miocene Bhuban and Boka Bil Sandsne Reservoirs of Titas-15 Well M. Mostafizur Rahman 1, Badrul Imam 1,

More information

Dissolution in vitro of mineral fibres. Examples.

Dissolution in vitro of mineral fibres. Examples. Dissolution in vitro of mineral fibres. Examples. Pacella A. Dipartimento di Scienze della Terra, Sapienza Università di Roma, Piazzale Aldo Moro 5, 00185 Roma, Italy European Mineralogical Union School

More information

Case Study: Tauhara New Zealand. Santiago de Chile, May 2014

Case Study: Tauhara New Zealand. Santiago de Chile, May 2014 Case Study: Tauhara New Zealand The Geothermal Institute University of Auckland Bridget Lynne Santiago de Chile, 26-29 May 2014 Bridget Y. Lynne Mick Pender Trystan Glynn-Morris Tauhara Subsidence Case

More information

ASBESTOS-CONTAINING MATERIAL FOR SURFACING APPLICATIONS (Adopted December 15, 1994; Amended March 21, 2002.)

ASBESTOS-CONTAINING MATERIAL FOR SURFACING APPLICATIONS (Adopted December 15, 1994; Amended March 21, 2002.) RULE 7050 ASBESTOS-CONTAINING MATERIAL FOR SURFACING APPLICATIONS (Adopted December 15, 1994; Amended March 21, 2002.) 1.0 Purpose The purpose of this rule is to control airborne emissions of asbestos

More information

Metcalf and Buck. GSA Data Repository

Metcalf and Buck. GSA Data Repository GSA Data Repository 2015035 Metcalf and Buck Figure DR1. Secondary ionization mass-spectrometry U-Pb zircon geochronology plots for data collected on two samples of Wilson Ridge plutonic rocks. Data presented

More information

MORTAR ANALYSIS REPORT. AP 2898 Cupar Stone Survey, Cupar

MORTAR ANALYSIS REPORT. AP 2898 Cupar Stone Survey, Cupar Charlestown Workshops 2 Rocks Road Charlestown Fife KY11 3EN T: + 44 (0)1383 872722 F: + 44 (0)1383 872744 Cupar Stone Survey, Cupar Bedding Mortar SCOTTISH LIME CENTRE TRUST is a charity registered in

More information

GEOL Lab 11 (Metamorphic Rocks in Hand Sample and Thin Section)

GEOL Lab 11 (Metamorphic Rocks in Hand Sample and Thin Section) GEOL 333 - Lab 11 (Metamorphic Rocks in Hand Sample and Thin Section) Introduction - Metamorphic rock forms from any pre-existing rock that undergoes changes due to intense heat and pressure without melting.

More information

ESS Minerals. Lee. 1. The table below shows some properties of four different minerals.

ESS Minerals. Lee. 1. The table below shows some properties of four different minerals. Name: ESS Minerals Pd. 1. The table below shows some properties of four different minerals. The minerals listed in the table are varieties of which mineral? (A) garnet (B) magnetite (C) olivine (D) quartz

More information

Igneous Rocks. Sedimentary Rocks. Metamorphic Rocks

Igneous Rocks. Sedimentary Rocks. Metamorphic Rocks Name: Date: Igneous Rocks Igneous rocks form from the solidification of magma either below (intrusive igneous rocks) or above (extrusive igneous rocks) the Earth s surface. For example, the igneous rock

More information

Pore Types Across Thermal Maturity: Eagle-Ford Formation, South Texas*

Pore Types Across Thermal Maturity: Eagle-Ford Formation, South Texas* Pore Types Across Thermal Maturity: Eagle-Ford Formation, South Texas* Maxwell E. Pommer 1, Kitty L. Milliken 1, and Aysen Ozkan 2 Search and Discovery Article #50987 (2014)** Posted July 24, 2014 *Adapted

More information

This document composed by: Hannu Luodes Geological Survey of Finland tel

This document composed by: Hannu Luodes Geological Survey of Finland tel This document composed by: Hannu Luodes Geological Survey of Finland Hannu.luodes@gtk.fi tel. +358 20550 3528 CONTENTS 1. GENERAL INFORMATION... 1 2. LOCATION OF THE QUARRY... 2 3. MINERALOGY... 3 3.1.

More information

Some Slides Lack Permission for Reproduction. These Slides must be deleted before posting as html or pdf! Metamorphic Rocks. GEOL 101 Lecture

Some Slides Lack Permission for Reproduction. These Slides must be deleted before posting as html or pdf! Metamorphic Rocks. GEOL 101 Lecture Some Slides Lack Permission for Reproduction. These Slides must be deleted before posting as html or pdf! Metamorphic Rocks GEOL 101 Lecture 9 2006 JS Kite WVU What is story behind this rock? Test 1 Results

More information

MINERALOGY LABORATORY Metamorphic Rocks and Minerals

MINERALOGY LABORATORY Metamorphic Rocks and Minerals Some of the samples used in Mineralogy Lab are museum specimens. Please do not destroy or heist them. You can do just about anything you want to the grungy ones, but be nice to the pretty specimens as

More information

Silica Distribution in Oxidized Biwabik Iron Formation: Ore-Waste Cutoff Prediction

Silica Distribution in Oxidized Biwabik Iron Formation: Ore-Waste Cutoff Prediction Journal of Undergraduate Research at Minnesota State University, Mankato Volume 13 Article 7 2013 Silica Distribution in Oxidized Biwabik Iron Formation: Ore-Waste Cutoff Prediction Ryan Rague Minnesota

More information

SUB-SURFACE GEOLOGY AND HYDROTHERMAL ALTERATION OF WELLS LA-9D AND LA-10D OF ALUTO LANGANO GEOTHERMAL FIELD, ETHIOPIA

SUB-SURFACE GEOLOGY AND HYDROTHERMAL ALTERATION OF WELLS LA-9D AND LA-10D OF ALUTO LANGANO GEOTHERMAL FIELD, ETHIOPIA Proceedings, 6 th African Rift Geothermal Conference Addis Ababa, Ethiopia, 2 nd -4 th November 2016 SUB-SURFACE GEOLOGY AND HYDROTHERMAL ALTERATION OF WELLS LA-9D AND LA-10D OF ALUTO LANGANO GEOTHERMAL

More information

Development of natural stone educational and research environment in East Finland

Development of natural stone educational and research environment in East Finland Development of natural stone educational and research environment in East Finland Geological Survey of Finland Eastern Finland Office P.O.Box 1237 70211 Kuopio Finland Tel. +358 205 5011 http://www.gtk.fi

More information

Lithology: Olivine-rich gabbro medium grained Observer: Texture: granular Ave. grain size: medium grained [345] Shape Habit Comments

Lithology: Olivine-rich gabbro medium grained Observer: Texture: granular Ave. grain size: medium grained [345] Shape Habit Comments THIN SECTION LABEL ID: 179-1105A-1R-2-W 88/91-TSB-TSS Piece no.: #02 TS no.: Igneous Medium-grained olivine gabbronorite; plagioclase chadacryst within orthopyroxene oikocryst; rims of olivine and clinopyroxene

More information

4. The diagram of Bowen's Reaction Series below indicates the relative temperatures at which specific minerals crystallize as magma cools.

4. The diagram of Bowen's Reaction Series below indicates the relative temperatures at which specific minerals crystallize as magma cools. 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. 1. The luster of this mineral could

More information

MINERALOGY AND CHEMISTRY OF MINE WASTE ROCK PILES IN MINING DISTRICTS IN SOUTHERN COLORADO AND NEW MEXICO

MINERALOGY AND CHEMISTRY OF MINE WASTE ROCK PILES IN MINING DISTRICTS IN SOUTHERN COLORADO AND NEW MEXICO MINERALOGY AND CHEMISTRY OF MINE WASTE ROCK PILES IN MINING DISTRICTS IN SOUTHERN COLORADO AND NEW MEXICO Virginia T. McLemore and Marcus Silva New Mexico Bureau of Geology and Mineral Resources, New Mexico

More information

BIO & PHARMA ANALYTICAL TECHNIQUES. Chapter 5 Particle Size Analysis

BIO & PHARMA ANALYTICAL TECHNIQUES. Chapter 5 Particle Size Analysis BIO & PHARMA ANALYTICAL TECHNIQUES Chapter 5 by Dr Siti Umairah Mokhtar Faculty of Engineering Technology umairah@ump.edu.my Chapter Description Aims Discuss theory, principles and application of analytical

More information

Version 1 Page 1 Barnard/George/Ward

Version 1 Page 1 Barnard/George/Ward The Great Mineral & Rock Test 1. Base your answer to the following question on the table below which provides information about the crystal sizes and the mineral compositions of four igneous rocks, A,

More information

EESC 4701: Igneous and Metamorphic Petrology IGNEOUS MINERALS LAB 1 HANDOUT

EESC 4701: Igneous and Metamorphic Petrology IGNEOUS MINERALS LAB 1 HANDOUT EESC 4701: Igneous and Metamorphic Petrology IGNEOUS MINERALS LAB 1 HANDOUT Sources: Cornell EAS302 lab, UMass Lowell 89.301 Mineralogy, LHRIC.org The Petrographic Microscope As you know, light is an electromagnetic

More information

ROCK CLASSIFICATION AND IDENTIFICATION

ROCK 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 information

RODINGITES IN THE LIZARD COMPLEX. by A. Hall. Department of Geology, King's College. Strand, London WC2R 2LS

RODINGITES IN THE LIZARD COMPLEX. by A. Hall. Department of Geology, King's College. Strand, London WC2R 2LS RODINGITES IN THE LIZARD COMPLEX by A. Hall Department of Geology, King's College. Strand, London WC2R 2LS Abstract. Rodingites are metasomatised rocks and veinstones that occur near the contacts of serpentinized

More information

Lab 6 - Identification of Metamorphic Rocks

Lab 6 - Identification of Metamorphic Rocks Lab 6 - Identification of Metamorphic Rocks Page - Introduction Metamorphic rocks are the third great rock group. The term meta means to change and morph means form. Metamorphic rocks are rocks who have

More information

The most common elements that make up minerals are oxygen, silicon, aluminum, iron, calcium, potassium, and magnesium

The most common elements that make up minerals are oxygen, silicon, aluminum, iron, calcium, potassium, and magnesium Mineralogy: The Study of Minerals and their Properties A Mineral! Occurs! Is a! Is a substance (element or compound)! Has atoms arrange in an orderly pattern ( )! Is (not formed by any process involving

More information

Determination of Reservoir Properties from XRF Elemental Data in the Montney Formation

Determination of Reservoir Properties from XRF Elemental Data in the Montney Formation Determination of Reservoir Properties from XRF Elemental Data in the Montney Formation Justin Besplug, Ron Spencer and Tom Weedmark - XRF Solutions - www.xrfsolutions.ca Abstract Portable X-Ray Fluorescence

More information

EESC 4701: Igneous and Metamorphic Petrology METAMORPHIC ROCKS LAB 8 HANDOUT

EESC 4701: Igneous and Metamorphic Petrology METAMORPHIC ROCKS LAB 8 HANDOUT Sources: Caltech, Cornell, UCSC, TAMIU Introduction EESC 4701: Igneous and Metamorphic Petrology METAMORPHIC ROCKS LAB 8 HANDOUT Metamorphism is the process by which physical and chemical changes in a

More information

Introducing the Morphologi G3 ID The future of particle characterization

Introducing the Morphologi G3 ID The future of particle characterization Introducing the Morphologi G3 ID The future of particle characterization Dr Anne Virden, Product technical specialist diffraction and analytical imaging What is the Morphologi G3-ID? Advanced R&D particle

More information

Pinchin Ltd. Asbestos Laboratory Certificate of Analysis

Pinchin Ltd. Asbestos Laboratory Certificate of Analysis M. Adams / B. Ficko Date Received: March 24, 2017 Lab Reference No.: b167122 Date Analyzed: March 25, 2017 Analyst(s): C. Luong / T. Ly # Samples submitted: 9 # Phases analyzed: 18 Method of Analysis:

More information

Geotechnical Engineering I CE 341

Geotechnical Engineering I CE 341 Geotechnical Engineering I CE 341 What do we learn in this course? Introduction to Geotechnical Engineering (1) Formation, Soil Composition, Type and Identification of Soils (2) Soil Structure and Fabric

More information

Sedimentary Rocks. Weathering. Mechanical & Chemical Weathering. Sediments. Lithification. Deposition. Transport. Erosion.

Sedimentary 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 information

An Investigation into

An Investigation into An Investigation into MINERALOGICAL CHARACTERIZATION OF FOUR TAILINGS SAMPLES prepared for LISHEEN MINE LR 11527-001 MI5002-APR07 May 28, 2007 NOTE: This report refers to the samples as received. The practice

More information

Suzanne Picazo, Mathilde Cannat, Adelie Delacour, Javier Escartın, Stephane Roumejon, and Serguei Silantyev

Suzanne Picazo, Mathilde Cannat, Adelie Delacour, Javier Escartın, Stephane Roumejon, and Serguei Silantyev Correction Volume 14, Number 8 16 August 2013 doi: ISSN: 1525-2027 Correction to Deformation associated with the denudation of mantle-derived rocks at the Mid- Atlantic Ridge 13 15 N: The role of magmatic

More information

Quartz. ! Naturally occurring - formed by nature. ! Solid - not liquid or gas. Liquid water is not a mineral

Quartz. ! Naturally occurring - formed by nature. ! Solid - not liquid or gas. Liquid water is not a mineral GEOL 110 - Minerals, Igneous Rocks Minerals Diamond Azurite Quartz Why Study Minerals?! Rocks = aggregates of minerals! Importance to Society?! Importance to Geology? 5 part definition, must satisfy all

More information

DISCOVERY OF MINERALISED PORPHYRY & MAGNETITE-COPPER-GOLD AT KAMARANGAN

DISCOVERY OF MINERALISED PORPHYRY & MAGNETITE-COPPER-GOLD AT KAMARANGAN MEDUSA MINING LIMITED ABN: 60 099 377 849 Unit 7, 11 Preston Street Como WA 6152 PO Box 860 Canning Bridge WA 6153 Telephone: +618-9367 0601 Facsimile: +618-9367 0602 Email: admin@medusamining.com.au Internet:

More information

Quantitative determination of common types of asbestos by diffuse reflectance FTIR using the Agilent Cary 630 Spectrometer

Quantitative determination of common types of asbestos by diffuse reflectance FTIR using the Agilent Cary 630 Spectrometer materials analysis Quantitative determination of common types of asbestos by diffuse reflectance FTIR using the Agilent Cary 630 Spectrometer Solutions for Your Analytical Business Markets and Applications

More information

INTERNATIONAL MODULE SYLLABUS W504 ASBESTOS AND OTHER FIBRES

INTERNATIONAL MODULE SYLLABUS W504 ASBESTOS AND OTHER FIBRES OHTA INTERNATIONAL MODULE SYLLABUS W504 ASBESTOS AND OTHER FIBRES Aim Learning Outcomes This module enhances the student s knowledge of occupational hygiene practice in relation to fibrous dusts. The module

More information

Minerals II: Physical Properties and Crystal Forms. From:

Minerals II: Physical Properties and Crystal Forms. From: Minerals II: Physical Properties and Crystal Forms From: http://webmineral.com/data/rhodochrosite.shtml The Physical Properties of Minerals Color Streak Luster Hardness External Crystal Form Cleavage The

More information

Geology and Petrography of Peridotites (Mantle Section) from Bela Ophiolite, Balochistan, Pakistan

Geology and Petrography of Peridotites (Mantle Section) from Bela Ophiolite, Balochistan, Pakistan Geology and Petrography of Peridotites (Mantle Section) from Bela Ophiolite, Balochistan, Pakistan Mehrab Khan, Muhammad Jahangir Khan Department of Earth & Environmental Sciences Bahria University Karachi

More information

Zusammenfassung der Ergebnisse SEMS 7 Scanning Electron Microscopy Scheme - Round 7

Zusammenfassung der Ergebnisse SEMS 7 Scanning Electron Microscopy Scheme - Round 7 Zusammenfassung der Ergebnisse SEMS 7 Scanning Electron Microscopy Scheme - Round 7 Ergebnisse CRB Ergebnisse Ringversuch Sample 1-7SEM1 [ fibres mm -2 ] Amphibole Chrysotile Other inorg. fibres Total

More information

Development of natural stone educational and research environment in East Finland

Development of natural stone educational and research environment in East Finland Development of natural stone educational and research environment in East Finland Geological Survey of Finland Eastern Finland Office P.O.Box 1237 70211 Kuopio Finland Tel. +358 205 5011 http://www.gtk.fi

More information

Scanning Electron Microscopy Scheme

Scanning Electron Microscopy Scheme Group Report Round 7A November 2017 Scanning Electron Microscopy Scheme BACKGROUND This report covers Round 7 of the SEMS asbestos fibre counting PT scheme. The scheme is operated by HSL, in collaboration

More information

Supplementary Information

Supplementary Information Supplementary Information Supplementary Figure 1. Simplified geological map of the western Alps. The location of the sampling area is indicated by the red star. A: Argentera massif; PM: Pelvoux Massif;

More information

Chapter - IV PETROGRAPHY. Petrographic studies are an integral part of any structural or petrological studies in

Chapter - IV PETROGRAPHY. Petrographic studies are an integral part of any structural or petrological studies in Chapter - IV PETROGRAPHY 4.1. Introduction Petrographic studies are an integral part of any structural or petrological studies in identifying the mineral assemblages, assigning nomenclature and identifying

More information

Lithological variation of Middle Bakken reservoirs in SE Saskatchewan: implications for optimizing multi-stage hydraulic fracturing

Lithological variation of Middle Bakken reservoirs in SE Saskatchewan: implications for optimizing multi-stage hydraulic fracturing Lithological variation of Middle Bakken reservoirs in SE Saskatchewan: implications for optimizing multi-stage hydraulic fracturing Hairuo Qing, Guoxiang Chi, Adam Sturiala Dept of Geology University of

More information

GY 302: Crystallography & Mineralogy

GY 302: Crystallography & Mineralogy UNIVERSITY OF SOUTH ALABAMA GY 302: Crystallography & Mineralogy Lecture 7a: Optical Mineralogy (two day lecture) Instructor: Dr. Douglas Haywick This Week s Agenda 1. Properties of light 2. Minerals and

More information

Introduction to Prospecting. Session Two Geology

Introduction to Prospecting. Session Two Geology Introduction to Prospecting Session Two Geology The Earth Earth is 4.6 billion years old (Ba). Bacteria & algae +3.5 Ba. Microscopic animals ~2 Ba. Animals ~600 million years (Ma) old. Mankind about 100,000

More information

Quartz Cementation in Mudrocks: How Common Is It?

Quartz Cementation in Mudrocks: How Common Is It? Quartz Cementation in Mudrocks: How Common Is It? Kitty L. Milliken Barnett Shale SE/CL image Woodford Shale SE/CL image Cements are Pore-filling Precipitates Specific definition differs with research

More information

Mineralogy of VAG mine waste: Eden, VT. Alyssa Findlay, Greg Druschel and John Hughes Department of Geology, University of Vermont

Mineralogy of VAG mine waste: Eden, VT. Alyssa Findlay, Greg Druschel and John Hughes Department of Geology, University of Vermont Mineralogy of VAG mine waste: Eden, VT Alyssa Findlay, Greg Druschel and John Hughes Department of Geology, University of Vermont Site Background Vermont Asbestos Group mine located in Eden and Lowell

More information

GY 402: Sedimentary Petrology

GY 402: Sedimentary Petrology UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 12: Petrology of Immature Siliciclastic Sed. Rocks Instructor: Dr. Douglas W. Haywick Last Time 1. Factors promoting beach development

More information

Igneous petrology EOSC 321 Laboratory 8: Intermediate and Felsic Volcanic Rocks. Pyroclastic Rocks

Igneous petrology EOSC 321 Laboratory 8: Intermediate and Felsic Volcanic Rocks. Pyroclastic Rocks 321 Lab 8 Instructor: L. Porritt - 1 - Igneous petrology EOSC 321 Laboratory 8: Intermediate and Felsic Volcanic Rocks. Pyroclastic Rocks Learning Goals. After this Lab, you should be able: Identify fine-grained

More information

GEOLOGY 333 LAB 5. Light Mechanics

GEOLOGY 333 LAB 5. Light Mechanics GEOLOGY 333 LAB 5 OPTICAL MICROSCOPY & MINERALS IN THIN SECTION Light Mechanics Light Waves: Visible light travels in waves, which have measurable wavelengths, frequencies, and velocities Wavelength (

More information

MINERALS Smith and Pun Chapter 2 ATOMIC STRUCTURE

MINERALS Smith and Pun Chapter 2 ATOMIC STRUCTURE MINERALS Smith and Pun Chapter 2 1 ATOMIC STRUCTURE 2 1 ATOMIC STRUCTURE (2) (See Smith and Pun, pages 29-35) ELEMENT: Substance that cannot be broken down into other substances by ordinary chemical methods

More information

A GENERAL LOCATION GUIDE FOR ULTRAMAFIC ROCKS IN CALIFORNIA - AREAS MORE LIKELY TO CONTAIN NATURALLY OCCURRING ASBESTOS.

A GENERAL LOCATION GUIDE FOR ULTRAMAFIC ROCKS IN CALIFORNIA - AREAS MORE LIKELY TO CONTAIN NATURALLY OCCURRING ASBESTOS. OPEN-FILE REPORT 000-19 A GENERAL LOCATION GUIDE FOR ULTRAMAFIC ROCKS IN CALIFORNIA - AREAS MORE LIKY TO CONTAIN NATURALLY OCCURRING ASBESTOS August, 000 DEPARTMENT OF CONSERVATION Division of Mines and

More information