'SQ Short Course Presented athe
|
|
- Agatha Craig
- 5 years ago
- Views:
Transcription
1 B r i n e s a n d E v a p o r i t e s
2 Short Course in Geology: Volume 3 Brines and Evaporites Peter Sonnenfeld and J.-P. Perthuisot 'SQ Short Course Presented athe 28th International Geological Congress Washington, D. C. American Geophysical Union, Washington, D.C.
3 Maria Luisa Crawford and Elaine Padovani Short Course Serie Editor Library of Congress Cataloging-in-Publication Data Sonnenfeld, Peter. Brines and evaporites. Bibliography: p. 1. Salt. 2. Evaporites. II. Title. QE S2S ISBN I. Perhuisot, J.-P. 552' Copyright 1989 by the American Geophysical Union, 2000 Florida Avenue, NW, Washington, DC 20009, U.S.A. Figures, tables, and short excerpts may be reprinted in scientific books and journals if the source is properly cited. Authorization to photocopy items for internal or personal use, or the internal or personal use of specific clients, is granted by the American Geophysical Union for libraries and other users registered with the Copyright Clearance Center (CCC) Transactional Reporting Service, provided that the base fee of $1.00 per copy plus $0.10 per page is paid directly to CCC, 21 Congress Street, Salem, MA /89/$ This consent does not extend to other kinds of copying, such as copying for creating new collective works or for resale. The reproduction of multiple copies and the use of full articles or the use of extracts, including figures and tables, for commercial purposes requires permission from AGU. Printed in the United States of America.
4 CONTENTS Part L Genesis of Evaporites P. Sonnenfeld Preface 3 Introduction 5 Climatological factors 5 Freeze-drying 6 Evaporation 6 Aridity 6 Air masses 8 Hydrography 9 The Coriolis effect 10 The entrance restriction 11 Brines 11 Density stratification 13 Radiation and thermal effects 14 Anions in the concentrating brine 15 Cation surplus in the brine 16 Complexing in the brine 17 Biota in hypersaline brines 17 Brines moving through evaporites 18 Evaporitic rocks 19 Non-marine evaporites 20 Groundwater precipitation 20 The polar environment 22 Subtropicalakes 23 Sebkhas 25 Marine evaporites 25 Evaporite-related marine carbonates 26 Marine gypsum 27 Celestite and barite 27 Marine halite 27 Marine potash salts 28 Marine magnesium salts 34 Substitutions 34 Accessories in marine evaporites 35 Siliciclastics 36 Base metals around evaporites 39 Organic matter in evaporites 40 Secondary alteration of marine evaporites Dehydration of gypsum 41 Sulfatization of potash beds 43 Further alterations 46 Basin configuration 46 Basin modelling 51 The bull's eye model 51 The tear-drop model 53 The open shelf model 53 The barred basin model 54 The reflux model 55 The deep basin model 55 The deep dry basin or giant flood model The synsedimentary subsidence model Conclusion 64 Acknowledgments iii
5 iv CONTENTS Part IL Recent Evaporites J P. Perthuisot 65 Preface 67 Abstract 69 Introduction 69 Main characteristics of modern evaporite basins 69 Conditions of evaporite formation 69 Tentative typology of present sites of evaporites 70 Salt precipitation 71 Salinity distribution and gradients 72 Rate of deposition of evaporites 72 The significance of water depth 73 Independence of evaporitic processes of depth of water 73 Consequences of a deep water body 73 Organic matter and evaporites 74 The origin of organic matter in paralic evaporite basins 74 Preservation of organic matter 75 Modern evaporite occurrences 80 Continental evaporitic areas 80 Groundwater precipitation: The pedological crusts 80 Intermittent lakes 80 Perennial lakes 85 Paralic evaporitic areas 92 Hydrophysical and hydrochemical arrangement of paralic areas Experimental models: Salinas 94 The evaporitic tidal flats 98 The role of evaporitic tidal flats (sebkhas) and their feeder lagoons Sporadically flooded basins 101 Evaporitic inlets 103 Paralic to deep basins with continuous seawater input 105 The necessity of a dynamic approach to evaporite deposits 116 Conclusion 116 Acknowledgments 118 Index of evaporitic minerals 119 References cited
6 LIST OF FIGURES 1. Relative humidity over saturated brines 2. Width of subtropical anticyclones 3. The Coriolis effect on inflow/outflow interfaces 4. Crusts in semi-arid soils 5. Primary precipitation curve 6. Precipitation paths in exposed and covered brines 7. ph of iron sulfide stability 8. Primary sylvite-carnallite relationship 9. Modes of alkane production 10. Gypsum and celestite solubility in NaCl-brines 11. Basin with limited subsidence 12. Areal extent of Permian Castile and Salado seas 13. The bull's eye pattern 14. The Kara Bogaz Gol 15. The Salina A-1 unit in the Michigan Basin 16. The tear-drop pattern 17. The open shelf model 18. The barred basin model 19. The reflux model 20. The deep basin model 21. Wilfarth's deep dry basin model 22. Upper Miocene halite distribution under the Mediterranean Sea 23. The synsedimentary subsidence model 24. Stages in the synsedimentary subsidence model 25. Organic matter production in terrestrial, paralic and marine settings 26. Paralic species distribution and quantitative variations of biota 27. Source rock potential of the proximal paralic area in a lagoon 28. Bathymetric map and water currents in Lake Melah (Algeria) 29. Content of organic matter in present Lake Melah sediments 30. Organic matter in present sediments of Bahirat el Biban 31. The sedimentological framework of the paralic setting 32. Comparison of brines in continental sebkha and paralic salt basin 33. The Sebkha Kourzia (Tunisia) 34. Composition of Sebkha Kourzia brines 35. Tentative reconstruction of the evolution of the Sebkha Kourzia basin 36. Setting and drainage area of the Dead Sea 37. Bathymetry of the Dead Sea 38. Temperature, density and salinity in the northern basin of the Dead Sea 39. Recent evolution of Dead Sea brines (northern basin) 40. The Kara Bogaz Gol 41. Lake Chad 42. The lakes of the Kanem Peninsula 43. Lake Liwa 44. Composition of the surficial evaporite crust in Lake Liwa 45. Salinity gradients in the paralic setting 46. Climatic conditions at Salin de Giraud 47. Brine movements in concentrators at Salin de Giraud 48. Brine densities in the Salin de Giraud salt works 49. Present sediments in the Salin de Giraud salt works 50. Plant associations in the Salin de Giraud salt works 51. Trucial Coast sebkha 52. Schematic section of Trucial Coast tidal sebkhas 53. Laguna Ojo de Liebre, Baja California, Mexico 54. Location and bathymetric map of Bahirat el Biban and Sebkha bou Jmel 55. Evolution of the ionic composition of brines in Sebkha bou Jmel
7 vi FIGURES AND TABLES 56. Map of the Mg/Ca ionic ratio of surficial waters in Bahirat el Biban 57. Total organicarbon content of surficial waters in Bahirat el Biban 58. Boccana de Virrila (Peru) 59. Khwar al Odeid (Qatar) 60. The salinity field at Khawr al Odeid 61. Lake Assal 62. The Sebkha el Melah 63. Geological map of the Sehkha el Melah and its surrounding area 64. Isobathic map of sedimentary infill in the Sebkha el Melah 65. Isobathic map of the Flandrian sequence in the Sebkha el Melah 66. Isopach map of the sulfate layer, Sebkha el Melah 67. Isopach map of the halite layer, Sebkha el Melah 68. Cross section of the sedimentary infill of the Sebkha el Melah 69. Block diagram of Sebkha el Melah 70. Development of Flandrian sedimentation in the Sebkha el Melah 71. Explanation of the "bull's eye" pattern of a paralic evaporitic basin 72. Size comparison between a present and an Upper Jurassic evaporite basin 73. Zones of restriction in the Triangulo de las Bermudas, Spain 74. Zones of restriction in the Baltic Sea LIST OF TABLES 1. Changing ion ratios in precipitating brines 2. Types of perennial water bodies 3. Data on Sebkah el Melah 3O 7O 115
Basement Geology of the Beardmore Glacier Region. Triassic Vertebrates in the Transantarctic Mountains
Basement Geology of the Beardmore Glacier Region John D. Gunner Triassic Vertebrates in the Transantarctic Mountains Edwin H. Colbert Forms and Fades of Vertebraria in Relation to Gondwana Coal James M.
More informationCoastal and Estuarine Studies
Coastal and Estuarine Studies Series Editors' Malcolm J. Bowman Christopher N.K. Gyre in Lake Biwa Reproduced with permission from Asahi Shinbun Coastal and Estuarine Studies 48 Setsuo Okuda, JOrg Imberger,
More informationCoastal and Estuarine Studies
Coastal and Estuarine Studies Series Editors: Malcolm J. Bowman Christopher N.K. Solinity: :. W', ter f'-,ß The mean salinity field for winter in the Western Mediterranean Sea, reconstructed from a climatological
More informationWater Science and Application 7. A Peculiar River. Geology, Geomorphology, and Hydrology of the Deschutes River, Oregon
Water Science and Application 7 A Peculiar River Geology, Geomorphology, and Hydrology of the Deschutes River, Oregon Water Science and Application 7 A Peculiar River Geology, Geomorphology, and Hydrology
More informationUnderstanding Earth Fifth Edition
Understanding Earth Fifth Edition Grotzinger Jordan Press Siever Chapter 5: SEDIMENTATION: Rocks Formed by Surface Processes Lecturer: H Mohammadzadeh Assistant professors, Department of Geology, FUM Copyright
More informationCoastal Oceanography. Coastal Oceanography. Coastal Waters
Coastal Oceanography Coastal Oceanography 95% of ocean life is in coastal waters (320 km from shore) Estuaries and wetlands are among most productive ecosystems on Earth Major shipping routes, oil and
More informationQuartz or opaline silica solubility
Quartz or opaline silica solubility The simplest process that might regulate the concentration of an element in solution is equilibrium with respect to a solid phase containing the element as a major component.
More informationBiology of the Antarctic Seas XIX
Biology of the Antarctic Seas XIX Physical Sciences OCEANOLOGY Joseph L. Reid, Editor OCEANOLOGY II: THE AUSTRALIAN- NEW ZEALAND SECTOR Dennis E. Hayes, Editor SNOW AND ICE STUDIES Malcolm Melior, Editor
More informationAtmospheric Halos and the Search for Angle x
Atmospheric Halos and the Search for Angle x Atmospheric Halos and the Search for Angle x WalterTape and Jarmo Moilanen S American Geophysical Union Washington, DC Published under the aegis of the AGU
More informationThe Nature and Timing of Orogenic Activity in the Caledonian Rocks of the British Isles
The Nature and Timing of Orogenic Activity in the Caledonian Rocks of the British Isles The Nature and Timing of Orogenic Activity in the Caledonian of the British Isles Rocks EDITED BY A. L. HARRIS University
More information(4) Give an example of important reactions that are responsible for the composition of river water.
Lecture 12 Global Biogeochemical Cycles (1) If rivers are the chief source of the dissolved salts in seawater, why is seawater not simply a concentrated version of average composition of all rivers? The
More informationThe Nature of Sedimentary Rocks
The Nature of Sedimentary Rocks Sedimentary rocks are composed of: Fragments of other rocks Chemical precipitates Organic matter or biochemically produced materials The Nature of Sedimentary Rocks Sedimentary
More informationLecture 11: Non-Carbonate Biogenic and Chemical Sedimentary Rocks
Lecture 11: Non-Carbonate Biogenic and Chemical Sedimentary Rocks Siliceous Sediments & Chert Phosphorites Evaporites Banded Iron Siliceous Sedimentary Rocks Fine-grained, dense, hard rocks composed predominantly
More informationEPS 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 informationLecture 13 More Surface Reactions on Mineral Surfaces. & Intro to Soil Formation and Chemistry
Lecture 13 More Surface Reactions on Mineral Surfaces & Intro to Soil Formation and Chemistry 3. charge transfer (e.g., ligand/donor sorption): Sorption involves a number of related processes that all
More informationLecture 6 - Determinants of Seawater Composition. Sets up electric dipole because O is more electronegative A o. Figure 3.
12.742 - Marine Chemistry Fall 2004 Lecture 6 - Determinants of Seawater Composition Prof. Scott Doney What is seawater? Water Dissolved inorganic salts (major ions) Trace species, organics, colloids,
More informationLab 7: Sedimentary Structures
Name: Lab 7: Sedimentary Structures Sedimentary rocks account for a negligibly small fraction of Earth s mass, yet they are commonly encountered because the processes that form them are ubiquitous in the
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 informationSEDIMENTARY BASINS BASIN TYPES ACCORDING TO TECTONIC. by Prof. Dr. Abbas Mansour
SEDIMENTARY BASINS BASIN TYPES ACCORDING TO TECTONIC by Prof. Dr. Abbas Mansour B. Convergent plate margins 10. STABLE CONTINENTAL INTERIOR BASIN E.g. Lake Eyre Basin Intracratonic (= within stable continental
More informationWhere is all the water?
Where is all the water? The distribution of water at the Earth's surface % of total Oceans 97.25 Ice caps and glaciers 2.05 Groundwater 0.68 Lakes 0.01 Soils 0.005 Atmosphere (as vapour) 0.001 Rivers 0.0001
More informationSci.tanta.edu.eg PALEOECOLOGY, GE 2218
Sci.tanta.edu.eg PALEOECOLOGY, GE 2218 Lec. 4 1 Biosphere Lithosphere Community Hydrosphere Atmosphere 2 1 Temperature Temperature range in the ocean is approximately 2 to 40 º C. Coldest waters are found
More informationLecture Outline Wednesday - Friday February 14-16, 2018
Lecture Outline Wednesday - Friday February 14-16, 2018 Quiz 2 scheduled for Friday Feb 23 (Interlude B, Chapters 6,7) Questions? Chapter 6 Pages of the Past: Sedimentary Rocks Key Points for today Be
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 informationEmulsions. Fundamentals and Applications in the Petroleum Industry
ADVANCES IN CHEMISTRY SERIES 231 Downloaded via 148.251.232.83 on July 23, 2018 at 08:49:52 (UTC). See https://pubs.acs.org/sharingguidelines for options on how to legitimately share published articles.
More information1. are most likely to study the images sent back from Mars. A. Astronomers B. Geologists C. Doctors D. Engineers
1. are most likely to study the images sent back from Mars. A. Astronomers B. Geologists C. Doctors D. Engineers 2. When did the Earth form? A. About 540 million years ago B. About 2.5 billion years ago
More informationContents. 1 Introduction Stable Isotopes
Contents 1 Introduction... 1 Part I Stable Isotopes 2 Isotope Geochemistry of Natural Waters... 11 2.1 Some Properties of Waters and Solutions... 11 2.1.1 The Notion of Activity and the Activity Coefficient...
More informationThe boundary between two formations (or any distinct layers) is called a contact. Sedimentary rocks cover 75% of continents.
Sedimentary Rocks Sedimentary rocks form at the Earth s surface through interactions of the hydrologic system and the crust. Fortunately, many of these processes are in operation today, and geologists
More informationGeostatistics for Environmental and Geotechnical Applications
STP 1283 Geostatistics for Environmental and Geotechnical Applications Shahrokh Rouhani, R. Mohan Srivastava, Alexander J. Desbarats, Marc V. Cromer, and A. Ivan Johnson, editors ASTM Publication Code
More informationEarth Science in the City' A Reader
Earth Science in the City' A Reader Grant Heiken Robert Fakundiny John Sutter Editors American Geophysical Union Washington, DC Published under the aegis of the AGU Books Board Jean-Louis Bougeret, Chair;
More informationLake Levels and Climate Change in Maine and Eastern North America during the last 12,000 years
Maine Geologic Facts and Localities December, 2000 Lake Levels and Climate Change in Maine and Eastern North America during the last 12,000 years Text by Robert A. Johnston, Department of Agriculture,
More informationChapter 8 Fetter, Applied Hydrology 4 th Edition, Geology of Groundwater Occurrence
Chapter 8 Fetter, Applied Hydrology 4 th Edition, 2001 Geology of Groundwater Occurrence Figure 8.42. Alluvial Valleys ground-water region. Fetter, Applied Hydrology 4 th Edition, 2001 Fetter, Applied
More informationWater-Soluble Polymers
Downloaded via 148.251.232.83 on October 17, 2018 at 02:44:30 (UTC). See https://pubs.acs.org/sharingguidelines for options on how to legitimately share published articles. Water-Soluble Polymers ADVANCES
More informationOrigin and Evolution of Formation Waters in the West-Central Part of the Alberta Basin
Page No. 004-1 Origin and Evolution of Formation Waters in the West-Central Part of the Alberta Basin Karsten Michael* University of Alberta, 1-26 ESB, Edmonton, AB T6G 2E3 karsten@ualberta.ca and Stefan
More informationSediment and Sedimentary rock
Sediment and Sedimentary rock Sediment: An accumulation of loose mineral grains, such as boulders, pebbles, sand, silt or mud, which are not cemented together. Mechanical and chemical weathering produces
More informationSedimentary Rocks and Processes
Sedimentary Rocks and Processes Weathering Sedimentary Processes Breakdown of pre-existing rock by physical and chemical processes Transport Movement of sediments from environments of relatively high potential
More informationRock Physics & Phase Relations
AGU Reference Shelf AGU Reference Shelf 3 Rock Physics & Phase Relations A Handbook of Physical Constants Thomas J. Ahrens, Published under the aegis of the AGU Books Board Library of Congress Cataloging-in-Publication
More informationPrentice Hall. Earth Science (AP-Honors), 12th Edition 2009, (Tarbuck/Lutgens) High School
Prentice Hall Earth Science (AP-Honors), 12th Edition 2009, (Tarbuck/Lutgens) High School C O R R E L A T E D T O Correlation to the Mississippi Curriculum Frameworks - Earth and Space Science (High School)
More informationCretaceous, Dakota Formation, Terra Cotta Member South Side of I-70, Salina County, Kansas
Cretaceous, Dakota Formation, Terra Cotta Member South Side of I-70, Salina County, Kansas Written By: Steven D.J. Baumann G-102010-1A Outcrop looking southeast Photo taken by: Steven Baumann on 10-20-2010
More informationThe physical breakdown and chemical alteration of rocks and minerals at or near Earth s surface.
The physical breakdown and chemical alteration of rocks and minerals at or near Earth s surface. The material that is chemically and mechanically weathered to yield sediment and soil. Regolith consisting
More informationEvaporite basins with emphasis on the Permian Zechstein
Evaporite basins with emphasis on the Permian Zechstein Kristin Börner Institute of Geology, University of Mining and Technology, Freiberg, Germany Abstract. This paper looks first at the distribution
More informationNC Earth Science Essential Standards
NC Earth Science Essential Standards EEn. 2.1 Explain how processes and forces affect the Lithosphere. EEn. 2.1.1 Explain how the rock cycle, plate tectonics, volcanoes, and earthquakes impact the Lithosphere.
More informationPre-Lab Reading Questions ES202
ES202 The are designed to encourage students to read lab material prior to attending class during any given week. Reading the weekly lab prior to attending class will result in better grade performance
More informationWeathering, Erosion, Deposition, and Landscape Development
Weathering, Erosion, Deposition, and Landscape Development I. Weathering - the breakdown of rocks into smaller particles, also called sediments, by natural processes. Weathering is further divided into
More information1. Introduction 2. Ocean circulation a) Temperature, salinity, density b) Thermohaline circulation c) Wind-driven surface currents d) Circulation and
1. Introduction 2. Ocean circulation a) Temperature, salinity, density b) Thermohaline circulation c) Wind-driven surface currents d) Circulation and climate change e) Oceanic water residence times 3.
More informationGEOLOGY MEDIA SUITE Chapter 5
UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 5 Sedimentation Rocks Formed by Surface Processes 2010 W.H. Freeman and Company Mineralogy of sandstones Key Figure 5.12
More informationSection 2.1 Ocean Basins. - Has helped determine where ocean basins are located. - Tectonic plates move changing the position of the continents.
Science 8 Unit 1: Water Systems on Earth Chapter 2: Oceans Control the Water Cycle Section 2.1 Ocean Basins Oceans are important because: 1. Primary water source for the water cycle 2. Control weather
More informationGeochemical mobility of chemical elements in saline lake systems in Khakassia (Russia)
Available online at www.sciencedirect.com Procedia Earth and Planetary Science 7 ( 2013 ) 325 329 Water Rock Interaction [WRI 14] Geochemical mobility of chemical elements in saline lake systems in Khakassia
More informationLaboratory Exercise #4 Geologic Surface Processes in Dry Lands
Page - 1 Laboratory Exercise #4 Geologic Surface Processes in Dry Lands Section A Overview of Lands with Dry Climates The definition of a dry climate is tied to an understanding of the hydrologic cycle
More informationSedimentary Environments Chapter 8
Sedimentary Environments Chapter 8 Does not contain complete lecture notes. To be used to help organize lecture notes and home/test studies. What is a sedimentary rock? Sedimentary rocks are products of
More informationGrade 8 Science. Unit 1: Water Systems on Earth Chapter 2
Grade 8 Science Unit 1: Water Systems on Earth Chapter 2 Oceans are important... 1. Primary water source for the water cycle 2. Control weather 3. Support diverse life 4. Provides humans with food, minerals,
More informationGeology Merit Badge Workbook
Merit Badge Workbook This workbook can help you but you still need to read the merit badge pamphlet. This Workbook can help you organize your thoughts as you prepare to meet with your merit badge counselor.
More informationSedimentary Rocks Chapter 6
Sedimentary Rocks Chapter 6 I. What is a sedimentary rock? A. Sedimentary rock 1) Rock made of detrital sediments (such as sand) or inorganic/organic chemical precipitates (such as calcite) 2) Detrital
More informationWeathering Cycle Teacher Notes
The Weathering Cycle Stages of the Weathering Cycle: 1. Carbon Dioxide and Water In clouds, carbon dioxide reacts with water to form a weak acid. H 2 O + CO 2 --> H 2 CO 3 H 2 CO 3 H + + HCO 3-2. Acid
More informationAeolian Environments. And Controls on Sedimentation. John Luchok, Kyle Balling, Cristopher Alvarez
Aeolian Environments And Controls on Sedimentation John Luchok, Kyle Balling, Cristopher Alvarez The Aeolian Environment Aeolian Processes - geologic activity with regards to wind Desert Environments (Hyper-Arid,
More informationFresh Waters. Linda Aspen-Baxter
Fresh Waters Linda Aspen-Baxter Published by Weigl Publishers Inc. 350 5 th Avenue, Suite 3304, PMB 6G New York, NY 10118-0069 Web site: www.weigl.com Copyright 2007 Weigl Publishers Inc. All rights reserved.
More informationChapter 10. Chapter Rocks and the Rock Cycle. Rocks. Section 1 Rocks and the Rock Cycle
Chapter 10 Rocks 1 Chapter 10 Section 1 Rocks and the Rock Cycle 2 10.1 Rocks and the Rock Cycle Magma is the parent material for all rocks. Once the magma cools and hardens, many changes can occur. Geology:
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 informationJochen Hoefs Stable Isotope Geochemistry
Jochen Hoefs Stable Isotope Geochemistry Springer-Verlag Berlin Heidelberg GmbH Jochen Hoefs Stable Isotope Geochemistry 4th, Completely Revised, Updated, and Enlarged Edition With 73 Figures and 22 Tables
More informationDiagenetic processes in the Cenozoic sedimentary formations associated with the Chicxulub Impact Crater, northwestern Yucatan Peninsula, Mexico
The Second International Conference on Saltwater Intrusion and Coastal Aquifers Monitoring, Modeling, and Management. Mérida, Yucatán, México, March 30 - April 2, 2003 Diagenetic processes in the Cenozoic
More informationSedimentary Basins. Gerhard Einsele. Springer-Verlag Berlin Heidelberg New York London Paris Tokyo Hong Kong Barcelona Budapest
Gerhard Einsele Sedimentary Basins Evolution, Facies, and Sediment Budget With 269 Figures Springer-Verlag Berlin Heidelberg New York London Paris Tokyo Hong Kong Barcelona Budapest Contents Part I Types
More informationSedimentology & Stratigraphy. Thanks to Rob Viens for slides
Sedimentology & Stratigraphy Thanks to Rob Viens for slides Sedimentology The study of the processes that erode, transport and deposit sediments Sedimentary Petrology The study of the characteristics and
More informationDepositional Environments. Depositional Environments
Depositional Environments Geographic area in which sediment is deposited Characterized by a combination of geological process & environmental conditions Depositional Environments Geological processes:
More informationChapter 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 informationAeolian Environments and Controls on Sedimentation. Alex Bryk, Ron Cash, Jacob Wikle, Rebecca Alberts
Aeolian Environments and Controls on Sedimentation Alex Bryk, Ron Cash, Jacob Wikle, Rebecca Alberts Aeolian dunes develop in desert systems where there is an abundance of sand-grade material available
More informationChapter 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 informationYear 6. Geography. Revision
Year 6 Geography Revision November 2017 Rivers and World knowledge How the water cycle works and the meaning of the terms evaporation, condensation, precipitation, transpiration, surface run-off, groundwater
More informationMulti-Scale and High-Contrast PDE: From Modelling, to Mathematical Analysis, to Inversion
577 Multi-Scale and High-Contrast PDE: From Modelling, to Mathematical Analysis, to Inversion Conference on Multi-Scale and High-Contrast PDE: From Modelling, to Mathematical Analysis, to Inversion June
More informationChapter 6 Pages of Earth s Past: Sedimentary Rocks
Chapter 6 Pages of Earth s Past: Sedimentary Rocks Introduction! Drilling into the bottom of the North Sea, we encounter: " Soft mud and loose sand, silt, pebbles, and shells. Then: " Similar materials
More informationCrust Elements. Elements of Earth. Minerals. Crystals. Interconnected Rocks and minerals Interior processes Erosion and deposition Water and air
Emily and Megan Earth System Science Interconnected Rocks and minerals Interior processes Erosion and deposition Water and air Made of atoms Earth is mostly iron, by weight Elements of Earth Made of atoms
More informationEarth Science 11: Earth Materials, Sedimentary Rocks
Name: Date: Earth Science 11: Earth Materials, Sedimentary Rocks Chapter 1, pages 56 to 66 2.4: Sedimentary Rocks Sedimentary Rock Formation All sedimentary rocks form through compaction and cementation
More informationEcoregions Glossary. 7.8B: Changes To Texas Land Earth and Space
Ecoregions Glossary Ecoregions The term ecoregions was developed by combining the terms ecology and region. Ecology is the study of the interrelationship of organisms and their environments. The term,
More informationNew Uses of Sulfur II
Downloaded via 148.251.232.83 on March 16, 2019 at 03:40:16 (UTC). See https://pubs.acs.org/sharingguidelines for options on how to legitimately share published articles. New Uses of Sulfur II New Uses
More informationThere are many different kinds of salt, but for simplicity sake, sodium chloride (NaCl) in particular will be the topic of discussion.
There are many different kinds of salt, but for simplicity sake, sodium chloride (NaCl) in particular will be the topic of discussion. NaCl comes from both natural and anthropogenic sources. Naturally
More informationEngineering Geology ECIV 2204
Engineering Geology ECIV 2204 Instructor : Dr. Jehad Hamad 2017-2016 Chapter (6) : Sedimentary Rocks Chapter 6: Sedimentary Rocks Chapter 6: Sedimentary Rocks Origin and nature of sedimentary rocks: Sedimentary
More informationEOSC : Petrology MID TERM minutes
EOSC 221.201: Petrology MID TERM 2-2013 30 minutes PART 1: Individual Exam (42 marks) FAMILY NAME: (please print) GIVEN NAME: (please print) STUDENT NUMBER: (print CLEARLY) INSTRUCTOR: Dr. Stuart Sutherland
More informationSedimentary Rocks. Origin, Properties and Identification. Physical Geology GEOL 101 Lab Ray Rector - Instructor
Sedimentary Rocks Origin, Properties and Identification Physical Geology GEOL 101 Lab Ray Rector - Instructor Sedimentary Rock Origin and Identification Lab Pre-Lab Internet Link Resources 1) http://www.rockhounds.com/rockshop/rockkey/index.html
More informationGrade 8 Science. Unit 1: Water Systems on Earth Chapter 1
Grade 8 Science Unit 1: Water Systems on Earth Chapter 1 Effects of Water? Churchill River Large Ocean Wave How do you use water? House Hold Use Personal Use Recreational Activities Water Distribution
More informationSetting the Stage 8/28/09 1. Review. Landscape history of WY. Climate, geology and vegetation patterns in Wyoming
Setting the Stage Climate, geology and vegetation patterns in Wyoming 8/28/09 1 Review Vegetation ecology has its roots in phytogeography: Observation and description of PATTERNS of plant species distributions
More information43 Misconceptions About Spiders: Teaching a Difficult Concept to Preschool and Elementary Children
1 Michigan s Ride on the North 5 38 American Plate 19 25 32 Quantitative and Qualitative Differences in Science Writing With a Writing Template Intervention The New Reality of Higher Education: Technology
More informationUNIT V WATER (OCEANS)
UNIT V WATER (OCEANS) This unit deals with Hydrological Cycle Oceans submarine relief; distribution of temperature and salinity; movements of ocean water-waves, tides and currents CHAPTER WATER (OCEANS)
More informationSalinity distribution in the Oceans
Salinity distribution in the Oceans Average practical salinity of open ocean waters 34.72 http://eps.mcgill.ca/~courses/c542/ 1/58 Salinity distribution in the Oceans Factors that control seawater salinity:
More informationOceans I Notes. Oceanography
Oceans I Notes Outlines on the front table Oceanography the science of our oceans that mixes biology, geology, chemistry, and physics (among other sciences) to unravel the mysteries of our seas. Divisions
More informationEPSc 116: Resources of the Earth. Lecture 24 on Ch. 9: Fertilizer and Chemical Minerals. Themes
EPSc 116: Resources of the Earth Lecture 24 on Ch. 9: Fertilizer and Chemical Minerals Themes Look at earth as a source of chemicals, rather than just metals 3 general groups of non-metals: fuels, fertilizer
More informationGY 111 Lecture Note Series Sedimentary Environments 4: Carbonates
GY 111 Lecture Notes D. Haywick (2008-09) 1 Lecture Goals A) Shelf Terminology B) Reefs, atolls and oolites C) Evaporites and evaporate basins GY 111 Lecture Note Series Sedimentary Environments 4: Carbonates
More informationSediments and. Sedimentary Rocks
Sediments and Sedimentary Rocks Bottom Line Sedimentary rocks form from particles accumulated in sedimentary layers Sedimentary layers can be formed by clastic or detrital particles (e.g., sand grains,
More information35th Annual GCSSEPM Foundation Bob F Perkins Research Conference 2016
35th Annual GCSSEPM Foundation Bob F Perkins Research Conference 2016 Mesozoic of the Gulf Rim and Beyond: New Progress in Science and Exploration of the Gulf of Mexico Basin Houston, Texas, USA 8 9 December
More informationName: Period: Date: ID: A. Circle the choice that best completes the statement or answers the question and write the letter on the blank.
Name: Period: _ Date: _ ID: A Unit 7 Practice Circle the choice that best completes the statement or answers the question and write the letter on the blank. 1. What term describes the movement of rock
More information12 10 8 6 4 2 0 40-50 50-60 60-70 70-80 80-90 90-100 Fresh Water What we will cover The Hydrologic Cycle River systems Floods Groundwater Caves and Karst Topography Hot springs Distribution of water in
More informationAssignment of the Glass Transition
STP 1249 Assignment of the Glass Transition Rickey J. Seyler, Editor ASTM Publication Code Number (PCN): 04-012490-50 ASTM 1916 Race Street Philadelphia, PA 19103 Printed in the U.S.A. Library of Congress
More informationSEDIMENTARY PHOSPHORITES: GENESIS, FACIES AND OCCURRENCE. Peter Berger Samantha Dwyer Jessica Hellwig Eric Obrock Kristin Read
SEDIMENTARY PHOSPHORITES: GENESIS, FACIES AND OCCURRENCE Peter Berger Samantha Dwyer Jessica Hellwig Eric Obrock Kristin Read Introduction Phosphogenesis & Deposystems Facies Case Studies: Western U.S.,
More informationGY 112L: Earth History
UNIVERSITY OF SOUTH ALABAMA GY 112L: Earth History Lab Lecture 1: Rock Review Instructor: Dr. Douglas W. Haywick Introductory Agenda 1. Contact info for D. Haywick 2. GY 112L Course Outline (syllabus)
More informationSurface Processes Focus on Mass Wasting (Chapter 10)
Surface Processes Focus on Mass Wasting (Chapter 10) 1. What is the distinction between weathering, mass wasting, and erosion? 2. What is the controlling force in mass wasting? What force provides resistance?
More informationPLATE TECTONICS THEORY
PLATE TECTONICS THEORY Continental drift Sea floor spreading CONTINENTAL DRIFT CONTINENTAL DRIFT 1. The fitness of continents and Continental Reconstruction Earth ~200 million years ago 1.1 Geometrical
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 informationTHE CHANGING SURFACE OF THE EARTH
THE CHANGING SURFACE OF THE EARTH Key words Drain geological agent weathering erosion Sediment deposition transport The landscape is a consequence of the action of two types of geological processes; internal
More informationWeathering Erosion and Deposition. Presented by Kesler Science
Weathering Erosion and Deposition Presented by Kesler Science Essential Questions: 1. What effects do weathering, erosion, and deposition have on the environment in ecoregions? Weathering Chemical and
More informationSedimentary Rocks. Origin, Properties and Identification. Physical Geology GEOL 100. Ray Rector - Instructor
Sedimentary Rocks Origin, Properties and Identification Physical Geology GEOL 100 Ray Rector - Instructor Sedimentary Rock Origin and Identification Lab Pre-Lab Internet Link Resources 1) http://www.rockhounds.com/rockshop/rockkey/index.html
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 informationComplex Geometry and Lie Theory
http://dx.doi.org/10.1090/pspum/053 Complex Geometry and Lie Theory Proceedings of Symposia in PURE MATHEMATICS Volume 53 Complex Geometry and Lie Theory James A. Carlson C. Herbert Clemens David R. Morrison
More informationThe World Ocean. Pacific Ocean 181 x 10 6 km 2. Indian Ocean 74 x 10 6 km 2. Atlantic Ocean 106 x 10 6 km 2
The World Ocean The ocean and adjacent seas cover 70.8% of the surface of Earth, an area of 361,254,000 km 2 Pacific Ocean 181 x 10 6 km 2 Indian Ocean 74 x 10 6 km 2 Atlantic Ocean 106 x 10 6 km 2 Oceanic
More information