PETROG. The best tool for digital petrography data collection, management, analysis, presentation and sharing

Size: px
Start display at page:

Download "PETROG. The best tool for digital petrography data collection, management, analysis, presentation and sharing"

Transcription

1 PETROG The best tool for digital petrography data collection, management, analysis, presentation and sharing

2 Core material is retrieved at great expense. It is needed both because we want to see for ourselves (i.e. ground-truth) that which otherwise we can only infer indirectly (by petrophysical logging, seismic survey, etc.) and because there are some things which can only be seen directly. Petrographic analysis is generally the only time a geologist looks at the rock to determine its composition. If we are only going to look at the rock once, we must do it right first time.

3 Looking down a microscope: Under the cross hair we see booky kaolinite filling a grain mouldic pore created by the dissolution of plagioclase feldspar. In a traditional petrographic report the reader would see only an image and possibly some small data parameters. In Petrog the image is connected to the description and to the exact point on the slide - and this is true for every point described on the slide.

4 How much of this information would be captured by a petrographer using a 20- channel point counter? 20 channels means that everything that can be said about the entire slide has to be one of 20 different pre-determined categories. If we have 5 different grains on the slide and 4 different clay overgrowths, that s 20 already, and we haven t begun to consider clay habit, let alone porosity,..

5 PETROG provides the ability to describe each point in one of hundreds of millions of different ways with an average of only 3-4 clicks of the mouse, in a matter of a few seconds.

6 In this case: a point on this slide could be described as: 1 st Click: Authigenic Kaolinite Group

7 2 nd Click: Platy Books 3 rd Click: Cementing

8 4 th Click: Grain Mouldic porosity 5 th Click: Filling pore 6 th Click: pore formed from dissolution of

9 7 th Click: Plagioclase detrital mineral

10 So what did we see at the data point (everything else is not relevant in a sampling based procedure): Authigenic kaolinite with a booky growth form filling a grain mouldic pore which was formed by the dissolution of plagioclase feldspar So we now have 3 elements involved in a diagenetic sequence with their relationships recorded.

11 A sequence of 7 quick clicks gives us: Mineralogy of the data point under the cross hair Morphological growth form(s) of the mineral Relationship & habits of this mineral to the adjacent rock elements Sequence of diagenetic events at this point

12 . and all data is immediately stored digitally and in a hierarchical form. This means that the petrographer can describe ALL of what s/he sees at the sampling point on the slide, not have to second-guess how the data will later be used and structure his limited data collection system to capture only those relevant data elements.

13 All data arranged hierarchically: Because the data are stored hierarchically in the PETROG database, the petrographer is free to log and describe exactly what s/he sees, knowing that the analyst or any subsequent user can see more detail or a summary as the context requires. For example, Allophane will be included in any report of Clay Minerals; the sum of all silicate materials will include Sheet Silicates, Double-Chain Silicates, etc.: the petrographer is not forced to describe the rock in terms which will be expected in the report.

14 The petrographer is more comfortable, looking at the monitor instead of changing eye focus repeatedly, so s/he can capture MORE DATA FASTER!

15

16 and once the data collection is complete, analysis is quick and simple, including all the tools one would expect, such as ternary plots as both interactive exploratory or analytical tools on screen and high quality reporting tools for printing hard copy or creating digital displays.

17 and analyses which make full use of the additional data collected, to estimate original mineralogy, analyse microporosity, compare with other available numerical data sources (such as core analysis and XRD) and many more interactive analyses or hard copy displays, which have hitherto not been possible in any repeatable, quantitative way.

18 Innovative data deserves innovative analysis:

19 PETROG integrates Quantitative Textural Analysis and Quantitative Compositional Analysis

20 The Images are an Integral Part of the Story The images collected during modal analysis are not only useful for reference or for QA but can also enhance the analysis in many ways, such as stitching them to make a composite which can be panned and zoomed to look at larger features. PETROG is the only system to integrate images and make them an integral part of petrography

21 Extending the Analysis Images are routinely used in general purpose image analysis software, but PETROG provides petrography-specific analyses, such as our patented colour-based discrimination method for porosity, carbonates etc.

22 PETROG The best tool for digital petrography data collection, management, analysis, presentation and sharing.

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

Leo G. Giannetta, Shane K. Butler, Nathan D. Webb Illinois State Geological Survey University of Illinois Urbana-Champaign

Leo G. Giannetta, Shane K. Butler, Nathan D. Webb Illinois State Geological Survey University of Illinois Urbana-Champaign Identification of Clay Microporosity in the Reservoir Characterization of the Cypress Sandstone: Implications for Petrophysical Analysis, Reservoir Quality, and Depositional Environment Leo G. Giannetta,

More information

Micro-Structural Rock Modeling: Methodology and Application in Formation Evaluation

Micro-Structural Rock Modeling: Methodology and Application in Formation Evaluation Micro-Structural Rock Modeling: Methodology and Application in Formation Evaluation Guodong Jin 1, Chun Lan 1, Wei Shao 1, and Songhua Chen 1, 2 1 Baker Hughes Incorporated, Houston, Texas, USA 2 Now at

More information

Using Clay Microporosity to Improve Formation Evaluation in Potential ROZs: Cypress Sandstone, Illinois Basin

Using Clay Microporosity to Improve Formation Evaluation in Potential ROZs: Cypress Sandstone, Illinois Basin Using Clay Microporosity to Improve Formation Evaluation in Potential ROZs: Cypress Sandstone, Illinois Basin Leo G. Giannetta, Nathan D. Webb, Shane K. Butler, and Nathan P. Grigsby Illinois State Geological

More information

MINERAL DISTRIBUTION IN RESERVOIR ROCKS AND ITS IMPACT ON ENHANCED OIL RECOVERY

MINERAL DISTRIBUTION IN RESERVOIR ROCKS AND ITS IMPACT ON ENHANCED OIL RECOVERY SCA2011-57 1/6 MINERAL DISTRIBUTION IN RESERVOIR ROCKS AND ITS IMPACT ON ENHANCED OIL RECOVERY James J. Howard and Gary L. Lovell ConocoPhillips This paper was prepared for presentation at the International

More information

Bikashkali Jana*, Sudhir Mathur, Sudipto Datta

Bikashkali Jana*, Sudhir Mathur, Sudipto Datta 10 th Biennial International Conference & Exposition P 354 Facies characterization of a low permeability Cretaceous clastic reservoir to understand reservoir spatial distribution in the Nagayalanka Field,

More information

2003 GCSSEPM Foundation Ed Picou Fellowship Grant for Graduate Studies in the Earth Sciences Recipient

2003 GCSSEPM Foundation Ed Picou Fellowship Grant for Graduate Studies in the Earth Sciences Recipient 2003 GCSSEPM Foundation Ed Picou Fellowship Grant for Graduate Studies in the Earth Sciences Recipient Tarek A. El Shayeb University of Texas at Austin Integrated reservoir characterization and 3-D diagenetic

More information

A BASE SYSTEM FOR MICRO TRAFFIC SIMULATION USING THE GEOGRAPHICAL INFORMATION DATABASE

A BASE SYSTEM FOR MICRO TRAFFIC SIMULATION USING THE GEOGRAPHICAL INFORMATION DATABASE A BASE SYSTEM FOR MICRO TRAFFIC SIMULATION USING THE GEOGRAPHICAL INFORMATION DATABASE Yan LI Ritsumeikan Asia Pacific University E-mail: yanli@apu.ac.jp 1 INTRODUCTION In the recent years, with the rapid

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

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

Igneous Rocks (Right Side Question)

Igneous Rocks (Right Side Question) Igneous Rocks (Right Side Question) Record the question in your notebook! Using your understanding of rock texture (grain size, grain shape, grain pattern), explain the process that you would use to determine

More information

EPS 50 Lab 4: Sedimentary Rocks

EPS 50 Lab 4: Sedimentary Rocks Name: EPS 50 Lab 4: Sedimentary Rocks Grotzinger and Jordan, Chapter 5 Introduction In this lab we will classify sedimentary rocks and investigate the relationship between environmental conditions and

More information

Chapter: Earth Materials

Chapter: Earth Materials Table of Contents Chapter: Earth Materials Section 1: Minerals Section 2: Igneous Rocks Section 3: Sedimentary Rocks Section 4: Metamorphic Rocks and the Rock Cycle 1 Minerals Common Elements Composition

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

ACTIVITIES OF BAPEX LABORATORY

ACTIVITIES OF BAPEX LABORATORY ACTIVITIES OF BAPEX LABORATORY HISTORY OF BAPEX LABORATORY During Pakistan period a Petroleum Laboratory was set up under OGDC During 70s & 80s Laboratory was developed under Directorate of Exploration

More information

SEDIMENTARY TEXTURES:

SEDIMENTARY TEXTURES: SEDIMENTARY TEXTURES: What are they? Grain size Grain shape Particle Surface texture Grain fabric Grain Size Depositional environment - subaerial, water depth, energy Sediment maturity - source, weathering

More information

Mercia Mudstone Formation, caprock to carbon capture and storage sites: petrophysical and petrological characteristics

Mercia Mudstone Formation, caprock to carbon capture and storage sites: petrophysical and petrological characteristics Mercia Mudstone Formation, caprock to carbon capture and storage sites: petrophysical and petrological characteristics 1: University of Liverpool, UK 2: University of Newcastle, UK 3: FEI, Australia 4:

More information

Student Exploration: Weathering

Student Exploration: Weathering Name: Date: Student Exploration: Weathering Vocabulary: abrasion, chemical weathering, clay formation, climate, dissolving, frost wedging, granite, limestone, mechanical weathering, rusting, sandstone,

More information

Chapter 4 Implications of paleoceanography and paleoclimate

Chapter 4 Implications of paleoceanography and paleoclimate Age ka / Chapter 4 Implications of paleoceanography and paleoclimate 4.1 Paleoclimate expression 4.2 Implications of paleocirculation and tectonics 4.3 Paleoenvironmental reconstruction MD05-2901 (Liu

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

A New Look at Analyzing Petrographic Data: The Fuzzy Logic Approach

A New Look at Analyzing Petrographic Data: The Fuzzy Logic Approach A New Look at Analyzing Petrographic Data: The Fuzzy Logic Approach Adwait ChawathJ, Maqsood Ali, Ahmed Ouenes, William Weiss New Mexico Petroleum Recovery Research Center New Mexico Institute of Mining

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

Core Technology for Evaluating the Bakken

Core 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 information

Preliminary report on the diagenesis of the Lower New Red Sandstone deposits from the Colebrooke Borehole, Devon

Preliminary report on the diagenesis of the Lower New Red Sandstone deposits from the Colebrooke Borehole, Devon Preliminary report on the diagenesis of the Lower New Red Sandstone deposits from the Colebrooke Borehole, Devon A.J. LEONARD Department of Geology, University of Exeter, North Park Road, Exeter, Devon

More information

Pore and Grain Geometry Analysis of Sandstone Reservoir Rocks from a Well of a Northern German Basin

Pore and Grain Geometry Analysis of Sandstone Reservoir Rocks from a Well of a Northern German Basin International Journal of Sciences: Basic and Applied Research (IJSBAR) ISSN 2307-4531 (Print & Online) http://gssrr.org/index.php?journal=journalofbasicandapplied ----------------------------------------------------------------------------------------------------------------

More information

A Color Atlas Of Carbonate Sediments And Rocks Under The Microscope By A. E. Adams

A Color Atlas Of Carbonate Sediments And Rocks Under The Microscope By A. E. Adams A Color Atlas Of Carbonate Sediments And Rocks Under The Microscope By A. E. Adams If looking for a book by A. E. Adams A Color Atlas of Carbonate Sediments and Rocks Under the Microscope in pdf format,

More information

GeoFlex. Quantitative cuttings analysis and imaging service

GeoFlex. Quantitative cuttings analysis and imaging service GeoFlex Quantitative cuttings analysis and imaging service Bring the cuttings characterization lab to the field with the GeoFlex* quantitative cuttings analysis and imaging service from Geoservices, a

More information

EARTH SCIENCE. Geology, the Environment and the Universe. Chapter 5: Igneous Rocks

EARTH SCIENCE. Geology, the Environment and the Universe. Chapter 5: Igneous Rocks EARTH SCIENCE Geology, the Environment and the Universe Chapter 5: Igneous Rocks CHAPTER 5 Igneous Rocks Section 5.1 What are igneous rocks? Section 5.2 Classification of Igneous Rocks Click a hyperlink

More information

Cement in Cambrian Sandstone : Assessing the Potential for the Generation of Respirable Silica

Cement in Cambrian Sandstone : Assessing the Potential for the Generation of Respirable Silica Cement in Cambrian Sandstone : Assessing the Potential for the Generation of Respirable Silica J. Brian Mahoney Kent M. Syverson Department of Geology University of Wisconsin-Eau Claire Geologic Setting

More information

STONE ANALYSIS & MATCHING REPORT AP 2898 Cupar Stone and Slate Survey, Freemason s Hall, Cupar

STONE ANALYSIS & MATCHING REPORT AP 2898 Cupar Stone and Slate Survey, Freemason s Hall, Cupar Charlestown Workshops 2 Rocks Road Charlestown Fife KY11 3EN T: + 44 (0)1383 872722 F: + 44 (0)1383 872744 STONE ANALYSIS & MATCHING REPORT Cupar Stone and Slate Survey, Freemason s Hall, Cupar Sample

More information

CO 2 -water-rock reactivity at hydrothermal temperatures: The BigRig2 experiment

CO 2 -water-rock reactivity at hydrothermal temperatures: The BigRig2 experiment CO 2 -water-rock reactivity at hydrothermal temperatures: The BigRig2 experiment C.A. ROCHELLE 1 *, K. BATEMAN 1, A. LACINSKA 1, D. WAGNER 1, J. LIONS 2 AND I. GAUS 2 1 British Geological Survey, Keyworth,

More information

1: Research Institute of Petroleum Industry, RIPI, Iran, 2: STATOIL ASA, Norway,

1: Research Institute of Petroleum Industry, RIPI, Iran, 2: STATOIL ASA, Norway, SCA2005-42 1/12 INTEGRATED ANALYSIS OF CORE AND LOG DATA TO DETERMINE RESERVOIR ROCK TYPES AND EXTRAPOLATION TO UNCORED WELLS IN A HETEROGENEOUS CLASTIC AND CARBONATE RESERVOIR A. M. Bagheri 1, B. Biranvand

More information

DIAGENESIS OF THE BAR AIL SANDSTONES

DIAGENESIS OF THE BAR AIL SANDSTONES CHAPTER-VII DIAGENESIS OF THE BAR AIL SANDSTONES 7.1 INTRODUCTION Diagenesis is any chemical, physical, or biological change undergone by sediment after its initial deposition and during and after its

More information

GEOLOGICAL LOG INTERPRETATION TUTORIAL

GEOLOGICAL 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 information

COMPARISON OF AUTHIGENIC MINERALS IN SANDSTONES AND INTERBEDDED MUDSTONES, SILTSTONES AND SHALES, EAST BERLIN FORMATION, HARTFORD BASIN, USA

COMPARISON OF AUTHIGENIC MINERALS IN SANDSTONES AND INTERBEDDED MUDSTONES, SILTSTONES AND SHALES, EAST BERLIN FORMATION, HARTFORD BASIN, USA , 39-61. ISSN 1011-3924 Printed in Ethiopia 2007 Chemical Society of Ethiopia COMPARISON OF AUTHIGENIC MINERALS IN SANDSTONES AND INTERBEDDED MUDSTONES, SILTSTONES AND SHALES, EAST BERLIN FORMATION, HARTFORD

More information

Rock Physics Perturbational Modeling: Carbonate case study, an intracratonic basin Northwest/Saharan Africa

Rock Physics Perturbational Modeling: Carbonate case study, an intracratonic basin Northwest/Saharan Africa Rock Physics Perturbational Modeling: Carbonate case study, an intracratonic basin Northwest/Saharan Africa Franklin Ruiz, Carlos Cobos, Marcelo Benabentos, Beatriz Chacon, and Roberto Varade, Luis Gairifo,

More information

An application of microscopic analyses in shale gas rock description

An application of microscopic analyses in shale gas rock description NAFTA-GAZ maj 2011 ROK LXVII Grzegorz Leśniak Oil and Gas Institute, Krakow An application of microscopic analyses in shale gas rock description Introduction As a standard procedure in the analyses of

More information

How many of these words can you explain?

How many of these words can you explain? How many of these words can you explain? Students will Define metamorphic rocks, Describe how they are classified, and give several examples; Describe the factors that influence the composition and texture

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

Geophysics and Mapping. presented by: Stephen Brown

Geophysics and Mapping. presented by: Stephen Brown Geophysics and Mapping presented by: Stephen Brown Recommended book for INIGEMM Geophysics for the mineral exploration geoscientist, by Michael Dentith and Stephen Mudge, Cambridge University Press, 2014.

More information

Petrographic Aspects of the Rotliegend of the Groningen field

Petrographic Aspects of the Rotliegend of the Groningen field Petrographic Aspects of the Rotliegend of the Groningen field Inventory and quick-look analysis of petrographic data from the Groningen field Clemens Visser Date November 2016 Editors Jan van Elk & Dirk

More information

PDF HOW DO CLASTIC SEDIMENTARY ROCKS FORM EBOOK

PDF HOW DO CLASTIC SEDIMENTARY ROCKS FORM EBOOK 06 February, 2018 PDF HOW DO CLASTIC SEDIMENTARY ROCKS FORM EBOOK Document Filetype: PDF 457.68 KB 0 PDF HOW DO CLASTIC SEDIMENTARY ROCKS FORM EBOOK The rock fragments that form clastic sedimentary rocks

More information

Concrete Technology Prof. B. Bhattacharjee Department of Civil Engineering Indian Institute of Science IIT Delhi. Lecture - 6 Aggregates (Size, Shape)

Concrete Technology Prof. B. Bhattacharjee Department of Civil Engineering Indian Institute of Science IIT Delhi. Lecture - 6 Aggregates (Size, Shape) Concrete Technology Prof. B. Bhattacharjee Department of Civil Engineering Indian Institute of Science IIT Delhi Lecture - 6 Aggregates (Size, Shape) Welcome to concrete technology module 2. Module 2 deals

More information

Seismic mapping of the Utsira Formation. Petrophysical interpretations and fracture gradient estimates.

Seismic mapping of the Utsira Formation. Petrophysical interpretations and fracture gradient estimates. Presentation March 4 th 2009 OG21 Innovation Seminar: TTA2 Exploration and reservoir Characterization Venue: StatoilHydro, Sandsli CO 2 Sequestration A geophysical and geological study related to CO 2

More information

13. Sedimentary Rocks I (p )

13. Sedimentary Rocks I (p ) 13. Sedimentary Rocks I (p. 194-208) Sediment Deposition Weathering results in rock being broken down into smaller fragments, called regolith. This regolith is then broken down to form soil. The regolith

More information

INACCESSIBLE POROSITY INSIGHT TO PORE DEVELOPMENT AND SOLUTIONS TO MICP DATA INTERPRETATION

INACCESSIBLE POROSITY INSIGHT TO PORE DEVELOPMENT AND SOLUTIONS TO MICP DATA INTERPRETATION SCA2016-048 1/6 INACCESSIBLE POROSITY INSIGHT TO PORE DEVELOPMENT AND SOLUTIONS TO MICP DATA INTERPRETATION Leśniak G. 1, Such P. 1, Komorowska K. 2 1 Oil and Gas Institute National Research Institute,

More information

Researches of sequestration. CO2 in case of laboratory experiment and natural analogues. Speaker : Pei-Hua Hsu

Researches of sequestration. CO2 in case of laboratory experiment and natural analogues. Speaker : Pei-Hua Hsu Researches of sequestration CO2 in case of laboratory experiment and natural analogues Speaker : Pei-Hua Hsu References Fischer, S., Liebscher A., Wandrey M., the CO2SINK Group (2010). CO2-brine-rock interaction

More information

Kinetics of the opal-a to opal-ct phase transition in low- and high-toc siliceous shale source rocks

Kinetics of the opal-a to opal-ct phase transition in low- and high-toc siliceous shale source rocks Kinetics of the opal-a to opal-ct phase transition in low- and high-toc siliceous shale source rocks Danica Dralus Stanford University, now at BP Mike Lewan USGS, Denver, CO (retired) Ken Peters Schlumberger,

More information

MINERALOGICAL ASSOCIATION OF CANADA CLAYS AND THE RESOURCE GEOLOGIST

MINERALOGICAL ASSOCIATION OF CANADA CLAYS AND THE RESOURCE GEOLOGIST MINERALOGICAL ASSOCIATION OF CANADA SHORT COURSE HANDBOOK VOLUME 7, MAY 1981 EDITED BY: F.J. LONGSTAFFE CLAYS AND THE RESOURCE GEOLOGIST A short course sponsored by the Mineralogical Association of Canada

More information

THE ROCK CYCLE & ROCKS. Subtitle

THE ROCK CYCLE & ROCKS. Subtitle THE ROCK CYCLE & ROCKS Subtitle 3. Three rocks that do not have minerals or are composed of nonmineral matter. Coal Pumuce Obsidian THE ROCK CYCLE Why do scientists study rocks? Rocks contain clues about

More information

LAB 3: COMMON MINERALS IN SEDIMENTARY ROCKS, Part 1

LAB 3: COMMON MINERALS IN SEDIMENTARY ROCKS, Part 1 EESC 2100: Mineralogy LAB 3: COMMON MINERALS IN SEDIMENTARY ROCKS, Part 1 Learning Objectives: Students will be able to identify minerals that occur commonly in sandstones (quartz and feldspars), both

More information

Integrating Geomechanics and Reservoir Characterization Examples from Canadian Shale Plays

Integrating Geomechanics and Reservoir Characterization Examples from Canadian Shale Plays Integrating Geomechanics and Reservoir Characterization Examples from Canadian Shale Plays AAPG Geosciences Technology Workshops Geomechanics and Reservoir Characterization of Shale and Carbonates July

More information

Geological Classification of Seismic-Inversion Data in the Doba Basin of Chad*

Geological Classification of Seismic-Inversion Data in the Doba Basin of Chad* Geological Classification of Seismic-Inversion Data in the Doba Basin of Chad* Carl Reine 1, Chris Szelewski 2, and Chaminda Sandanayake 3 Search and Discovery Article #41899 (2016)** Posted September

More information

The effect of CO 2 -fluid-rock interactions on the porosity and permeability of calcite-bearing sandstone

The effect of CO 2 -fluid-rock interactions on the porosity and permeability of calcite-bearing sandstone The effect of CO 2 -fluid-rock interactions on the porosity and permeability of calcite-bearing sandstone Benoit Lamy-Chappuis, Bruce Yardley, Carlos Grattoni School of Earth and Environment, University

More information

INTRODUCTION TO WELL LOGS And BAYES THEOREM

INTRODUCTION TO WELL LOGS And BAYES THEOREM INTRODUCTION TO WELL LOGS And BAYES THEOREM EECS 833, 7 February 006 Geoff Bohling Assistant Scientist Kansas Geological Survey geoff@kgs.ku.edu 864-093 Overheads and resources available at http://people.ku.edu/~gbohling/eecs833

More information

A Joint European GIS Under Construction: The 1:5 Million International Geological Map of Europe and Adjacent Areas (IGME 5000)

A Joint European GIS Under Construction: The 1:5 Million International Geological Map of Europe and Adjacent Areas (IGME 5000) Abstract 2001 Annual Conference of the International Association for Mathematical Geology Technical Program - Session I (Poster) Building National and Regional Geologic Map Databases A Joint European GIS

More information

9/4/2015. Feldspars White, pink, variable Clays White perfect Quartz Colourless, white, red, None

9/4/2015. Feldspars White, pink, variable Clays White perfect Quartz Colourless, white, red, None ENGINEERING GEOLOGY Chapter 1.0: Introduction to engineering geology Chapter 2.0: Rock classification Igneous rocks Sedimentary rocks Metamorphic rocks Chapter 3.0: Weathering & soils Chapter 4.0: Geological

More information

A COMPARATIVE STUDY OF SHALE PORE STRUCTURE ANALYSIS

A COMPARATIVE STUDY OF SHALE PORE STRUCTURE ANALYSIS SCA2017-092 1 of 9 A COMPARATIVE STUDY OF SHALE PORE STRUCTURE ANALYSIS R. Cicha-Szot, P. Budak, G. Leśniak, P. Such, Instytut Nafty i Gazu - Państwowy Instytut Badawczy, Kraków, Poland This paper was

More information

Tu E Understanding Net Pay in Tight Gas Sands - A Case Study from the Lower Saxony Basin, NW- Germany

Tu E Understanding Net Pay in Tight Gas Sands - A Case Study from the Lower Saxony Basin, NW- Germany Tu E103 06 Understanding Net Pay in Tight Gas Sands - A Case Study from the Lower Saxony Basin, NW- Germany B. Koehrer* (Wintershall Holding GmbH), K. Wimmers (Wintershall Holding GmbH) & J. Strobel (Wintershall

More information

Minerals and Rocks. Environmental Learning Community CORC 1332 Sept 21, 2010

Minerals and Rocks. Environmental Learning Community CORC 1332 Sept 21, 2010 Minerals and Rocks Environmental Learning Community CORC 1332 Sept 21, 2010 Outline Quiz More on minerals Twinkies Rocks How can you identify one mineral from another? Distinguishing One Mineral from Another

More information

MAGNETIC SUSCEPTIBILITY OF DRILL CUTTINGS IN A NORTH SEA OIL WELL: A RAPID, NON- DESTRUCTIVE MEANS OF CHARACTERIZING LITHOLOGY

MAGNETIC SUSCEPTIBILITY OF DRILL CUTTINGS IN A NORTH SEA OIL WELL: A RAPID, NON- DESTRUCTIVE MEANS OF CHARACTERIZING LITHOLOGY SCA2015-036 1/6 MAGNETIC SUSCEPTIBILITY OF DRILL CUTTINGS IN A NORTH SEA OIL WELL: A RAPID, NON- DESTRUCTIVE MEANS OF CHARACTERIZING LITHOLOGY 1 Arfan Ali, 2 David K. Potter and 3 Andrew Tugwell 1 Shell

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

Name Class Date. Chapter 3 Rocks Chapter Test. Write the letter that best answers the question or completes the statement on the line provided.

Name Class Date. Chapter 3 Rocks Chapter Test. Write the letter that best answers the question or completes the statement on the line provided. Chapter 3 Rocks Chapter Test Multiple Choice Write the letter that best answers the question or completes the statement on the line provided. 1. Which of the following is true about rocks? a. Rocks are

More information

GY 302: Crystallography & Mineralogy

GY 302: Crystallography & Mineralogy UNIVERSITY OF SOUTH ALABAMA GY 302: Crystallography & Mineralogy Lecture 7b: Optical Mineralogy Instructor: Dr. Douglas Haywick Last Time 1. Properties of light 2. Minerals and light transmission Light

More information

Sandstone Thin-Section Lab

Sandstone Thin-Section Lab Overview In this week's lab, you will learn the basics of the description and interpretation of sandstones in thin section. For each of the ten samples listed below, you should describe the following:

More information

Reservoir Quality Analysis of Sandstone & Carbonate Rock-Types

Reservoir Quality Analysis of Sandstone & Carbonate Rock-Types An Intensive 5 Day Training Course Reservoir Quality Analysis of Sandstone & Carbonate 14-18 Oct 2018, Dubai 02-NOV-17 This course is Designed, Developed, and will be Delivered under iso Quality Standards

More information

This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and

This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution

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

Pore Morphometrics and Thermal Evolution of Organic-Matter Microporosity, Colorado Group, Western Canada Sedimentary Basin

Pore Morphometrics and Thermal Evolution of Organic-Matter Microporosity, Colorado Group, Western Canada Sedimentary Basin Pore Morphometrics and Thermal Evolution of Organic-Matter Microporosity, Colorado Group, Western Canada Sedimentary Basin Peng Jiang*, Department of Earth Sciences, Western University, London, Ontario

More information

Petrology and Petrophysics of the Lance Formation (Upper Cretaceous), American Hunter, Old Road Unit 1, Sublette County, Wyoming

Petrology and Petrophysics of the Lance Formation (Upper Cretaceous), American Hunter, Old Road Unit 1, Sublette County, Wyoming CHAPTER 11 Petrology and Petrophysics of the Lance Formation (Upper Cretaceous), American Hunter, Old Road Unit 1, Sublette County, Wyoming J. C. WEBB The Discovery Group, Inc., Denver, Colorado, U.S.A.

More information

WHAT'S NEW IN HSC CHEMISTRY 6.0

WHAT'S NEW IN HSC CHEMISTRY 6.0 What's New in HSC 6.0 6-1 WHAT'S NEW IN HSC CHEMISTRY 6.0 Fig. 1. HSC Chemistry 6.0 Main Menu. The old HSC Chemistry 5.1 software is made for the simulation and modeling of single chemical reactions and

More information

Reservoir Rock Properties

Reservoir Rock Properties Reservoir Rock Properties From here on, sedimentology and petrophysics are important for a good understanding of the course material. I realize that not everybody has a solid background in these fields,

More information

Comparison of rock pore space based on X-ray computed microtomography (micro-ct) and nuclear magnetic resonance (NMR) data.

Comparison of rock pore space based on X-ray computed microtomography (micro-ct) and nuclear magnetic resonance (NMR) data. NAFTA-GAZ październik 2011 ROK LXVII Jadwiga Zalewska, Marek Dohnalik Oil and Gas Institute, Krakow Comparison of rock pore space based on X-ray computed microtomography (micro-ct) and nuclear magnetic

More information

Metamorphism occurs where equi P-T is disturbed

Metamorphism occurs where equi P-T is disturbed Metamorphism occurs where equi P-T is disturbed Steady-state geotherms are disturbed by a variety of processes including plate-tectonic transport of rocks and heat input by intrusion of magma active transport

More information

23/9/2013 ENGINEERING GEOLOGY. Chapter 2: Rock classification:

23/9/2013 ENGINEERING GEOLOGY. Chapter 2: Rock classification: ENGINEERING GEOLOGY Chapter 2: Rock classification: ENGINEERING GEOLOGY Chapter 1.0: Introduction to engineering geology Chapter 2.0: Rock classification Igneous rocks Sedimentary rocks Metamorphic rocks

More information

Petrophysical Rock Typing: Enhanced Permeability Prediction and Reservoir Descriptions*

Petrophysical Rock Typing: Enhanced Permeability Prediction and Reservoir Descriptions* Petrophysical Rock Typing: Enhanced Permeability Prediction and Reservoir Descriptions* Wanida Sritongthae 1 Search and Discovery Article #51265 (2016)** Posted June 20, 2016 *Adapted from oral presentation

More information

MAGNETIC SUSCEPTIBILITY AS A RAPID, NON- DESTRUCTIVE TECHNIQUE FOR IMPROVED RCAL AND SCAL PARAMETER PREDICTION

MAGNETIC SUSCEPTIBILITY AS A RAPID, NON- DESTRUCTIVE TECHNIQUE FOR IMPROVED RCAL AND SCAL PARAMETER PREDICTION SCA2005-02 1/13 MAGNETIC SUSCEPTIBILITY AS A RAPID, NON- DESTRUCTIVE TECHNIQUE FOR IMPROVED RCAL AND SCAL PARAMETER PREDICTION David K. Potter Institute of Petroleum Engineering, Heriot-Watt University,

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

Ingrain Laboratories INTEGRATED ROCK ANALYSIS FOR THE OIL AND GAS INDUSTRY

Ingrain Laboratories INTEGRATED ROCK ANALYSIS FOR THE OIL AND GAS INDUSTRY Ingrain Laboratories INTEGRATED ROCK ANALYSIS FOR THE OIL AND GAS INDUSTRY 3 INGRAIN We Help Identify and Develop the Most Productive Reservoir by Characterizing Rocks at Pore Level and Upscaling to the

More information

Microscopic and X-ray fluorescence researches on sandstone from Shahejie Formation, China

Microscopic and X-ray fluorescence researches on sandstone from Shahejie Formation, China IOSR Journal of Engineering (IOSRJEN) ISSN (e): 2250-3021, ISSN (p): 2278-8719 Vol. 06, Issue 04 (April. 2016), V2 PP 27-32 www.iosrjen.org Microscopic and X-ray fluorescence researches on sandstone from

More information

RAPID ESTIMATION OF HYDRAULIC FLOW UNIT PARAMETERS RQI AND FZI FROM MAGNETIC MEASUREMENTS IN SOME SHOREFACE RESERVOIRS

RAPID ESTIMATION OF HYDRAULIC FLOW UNIT PARAMETERS RQI AND FZI FROM MAGNETIC MEASUREMENTS IN SOME SHOREFACE RESERVOIRS SCA206-057 /6 RAPID ESTIMATION OF HYDRAULIC FLOW UNIT PARAMETERS RQI AND FZI FROM MAGNETIC MEASUREMENTS IN SOME SHOREFACE RESERVOIRS Carl Egiebor and David K. Potter Department of Physics, University of

More information

SCAL, Inc. Services & Capabilities

SCAL, Inc. Services & Capabilities SCAL, Inc. Services & Capabilities About Us 30 years of service 2019 marks the 30th year in operation for Midlandbased Special Core Analysis Laboratories, Inc. (SCAL, Inc.). We're proud to celebrate this

More information

Sedimentología Ayudantía Lectura 1 Carbonate minerals

Sedimentología Ayudantía Lectura 1 Carbonate minerals Carbonate minerals The most common minerals in this group are the calcium carbonates, calcite and aragonite, while dolomite (a magnesium calcium carbonate) and siderite (iron carbonate) are also frequently

More information

Minerals and Rocks. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left.

Minerals and Rocks. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left. Minerals and Rocks Chapter Test A Multiple Choice Write the letter of the correct answer on the line at the left. 1. An example of a mineral made up of a pure element is a. coal. b. copper. c. quartz.

More information

EOR BY ALKALI FLOODING IN THE VIENNA BASIN: FIRST EXPERIMENTAL RESULTS OF ALKALI/MINERAL REACTIONS IN RESERVOIR ROCKS

EOR BY ALKALI FLOODING IN THE VIENNA BASIN: FIRST EXPERIMENTAL RESULTS OF ALKALI/MINERAL REACTIONS IN RESERVOIR ROCKS SCA2017-053 1/10 EOR BY ALKALI FLOODING IN THE VIENNA BASIN: FIRST EXPERIMENTAL RESULTS OF ALKALI/MINERAL REACTIONS IN RESERVOIR ROCKS Wolfgang Hujer 1 ; Verena Leitenmüller 2, Kenny Walrond 2 1 OMV UPSTREAM

More information

The Sleipner Effect: a subtle relationship between the distribution of diagenetic clay, reservoir porosity, permeability, and water saturation

The Sleipner Effect: a subtle relationship between the distribution of diagenetic clay, reservoir porosity, permeability, and water saturation Clay Minerals (2000) 35, 185±200 The Sleipner Effect: a subtle relationship between the distribution of diagenetic clay, reservoir porosity, permeability, and water saturation P. H. NADEAU* Statoil a.s,

More information

Petrophysics Designed to Honour Core Duvernay & Triassic

Petrophysics Designed to Honour Core Duvernay & Triassic Petrophysics Designed to Honour Core Duvernay & Triassic Robert V. Everett Robert V. Everett Petrophysics Inc. Mike Berhane Alberta Geological Survey, AER Tristan Euzen IFP Technologies (Canada) Inc. James

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

LAB 9: ULTRAMAFIC ROCKS, CUMULATES AND MELT SOURCES

LAB 9: ULTRAMAFIC ROCKS, CUMULATES AND MELT SOURCES Geology 316 (Petrology) (03/26/2012) Name LAB 9: ULTRAMAFIC ROCKS, CUMULATES AND MELT SOURCES INTRODUCTION Ultramafic rocks are igneous rocks containing less than 10% felsic minerals (quartz + feldspars

More information

Clay Minerals and its importance on Hydrocarbon Production Potential in a part of Geleki oilfield of Upper Assam Basin

Clay Minerals and its importance on Hydrocarbon Production Potential in a part of Geleki oilfield of Upper Assam Basin Clay Minerals and its importance on Hydrocarbon Production Potential in a part of Geleki oilfield of Upper Assam Basin Minati Das 1 Professor Department of Petroleum Technology Dibrugarh University Dibrugarh-

More information

Texture. As A Facies Element. The Geometrical aspects of the component particles of a rock. Basic Considerations

Texture. As A Facies Element. The Geometrical aspects of the component particles of a rock. Basic Considerations Texture As A Facies Element The Geometrical aspects of the component particles of a rock. Includes: 1. Size of particles 2. Shape of particles 3. Fabric (arrangement) of particles Basic Considerations

More information

EPSC 445: Metamorphic Petrology Lecture 1: An introduction to metamorphism

EPSC 445: Metamorphic Petrology Lecture 1: An introduction to metamorphism EPSC 445: Metamorphic Petrology Lecture 1: An introduction to metamorphism Vincent van Hinsberg Department of Earth and Planetary Sciences, McGill University, Montréal, Québec, Canada Course practicalities

More information

GY 111 Lecture Notes Metamorphism 2: Regional Metamorphism

GY 111 Lecture Notes Metamorphism 2: Regional Metamorphism GY 111 Lecture Notes D. Haywick (2008-09) 1 Lecture Goals: A) Foliated rocks part 1 B) Folitaed rocks part 2 c) Non-foliated rocks GY 111 Lecture Notes Metamorphism 2: Regional Metamorphism Reference:

More information

INVESTIGATING DEVIATIONS FROM OVERALL POROSITY PERMEABILITY TRENDS

INVESTIGATING DEVIATIONS FROM OVERALL POROSITY PERMEABILITY TRENDS PROCEEDINGS, Thirty-Sixth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, January 30 - February 1, 2012 SGP-TR-194 INVESTIGATING DEVIATIONS FROM OVERALL POROSITY

More information

ABSTRACT SCA /6

ABSTRACT SCA /6 SCA2014-056 1/6 POSIBILITIES OF QUANTITATIVE EVALUATION OF POLISH SHALE-GAS ROCKS PETROPHYSICAL AND GEOMECHANICAL PARAMETERS BY LABORATORY ANALYTICAL METHODS AND WELL LOGS INTERPRETATION G. Leśniak 1,

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

GEOL FORENSIC GEOLOGY ROCK IDENTIFICATION

GEOL FORENSIC GEOLOGY ROCK IDENTIFICATION GEOL.2150 - FORENSIC GEOLOGY ROCK IDENTIFICATION Name I. Introduction There are three basic types of rocks - igneous, sedimentary, and metamorphic: Igneous. Igneous rocks have solidified from molten matter

More information

Lecture 6. Physical Properties. Solid Phase. Particle Composition

Lecture 6. Physical Properties. Solid Phase. Particle Composition Lecture 6 Physical Properties Solid Phase Particle Composition 1 Questions What are tetrahedrons and octahedrons? How do silica tetrahedra bonds affect mineral weathering? Difference between primary and

More information

ROCK PHYSICS DIAGNOSTICS OF NORTH SEA SANDS: LINK BETWEEN MICROSTRUCTURE AND SEISMIC PROPERTIES ABSTRACT

ROCK PHYSICS DIAGNOSTICS OF NORTH SEA SANDS: LINK BETWEEN MICROSTRUCTURE AND SEISMIC PROPERTIES ABSTRACT ROCK PHYSICS DIAGNOSTICS OF NORTH SEA SANDS: LINK BETWEEN MICROSTRUCTURE AND SEISMIC PROPERTIES PER AVSETH, JACK DVORKIN, AND GARY MAVKO Department of Geophysics, Stanford University, CA 94305-2215, USA

More information

Questions on the characteristics and generation of subduction-related andesitic magmas at convergent margins (not covered on Midterm exam)

Questions on the characteristics and generation of subduction-related andesitic magmas at convergent margins (not covered on Midterm exam) Study Guide for GEOL 285 - Petrology Final Exam Fall 2005 The exam will be held at 8-10 am, Wednesday, Dec. 14, 2005 in Room 310, White Hall will be available to answer questions on Monday, Dec. 12, and

More information