Explanatory Notes for the Vocabulary
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Lithologic Description of a Sediment Core from Round
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY LITHOLOGIC DESCRIPTION OF A SEDIMENT CORE FROM ROUND LAKE, KLAMATH COUNTY, OREGON David P. Adam1 Hugh J. Rieck2 Mary McGann1 Karen Schiller1 Andrei M. Sarna-Wojcicki1 U.S. GEOLOGICAL SURVEY OPEN-FILE REPORT 95-33 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 'Menlo Park, CA 94025 2Flagstaff, AZ 86001 Introduction As part of a series of investigations designed to study the Quaternary climatic histories of the western U.S. and the adjacent northeastern Pacific Ocean, a sediment core was collected from Round Lake, Klamath County, Oregon, in the fall of 1991. This report presents basic data concerning the Round Lake site, as well as lithologic descriptions of the recovered sediments. The drilling methods and core sampling and curation techniques used are described by Adam (1993). Acknowledgement Coring at Round Lake was made possible by the gracious cooperation of Mr. Les Northcutt, the owner of the property. Site description Round Lake is a broad open valley about 2.5 km wide and 5 km long that lies just west of the southern end of Upper Klamath Lake, Oregon (Figure 1), at an elevation of about 1300 meters. The basin is one of a series of northwest-southeast trending basins that also includes the Klamath graben and Long Lake. Regional bedrock consists of basalt and basaltic andesites of Pliocene and upper Miocene age (Walker and McLeod, 1991; Sherrod and Pickthorn, 1992). -
Sequence Stratigraphy of the Neoproterozoic Infra Krol Formation and Krol Group, Lesser Himalaya, India
SEQUENCE STRATIGRAPHY OF THE NEOPROTEROZOIC INFRA KROL FORMATION AND KROL GROUP, LESSER HIMALAYA, INDIA GANQING JIANG1, NICHOLAS CHRISTIE-BLICK1, ALAN J. KAUFMAN2, DHIRAJ M. BANERJEE3, AND VIBHUTI RAI4 1 Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964±8000, U.S.A. 2 Department of Geology, University of Maryland, College Park, Maryland 20742±4211, U.S.A. 3 Department of Geology, University of Delhi, Delhi 110007, India 4 Department of Geology, Lucknow University, Lucknow 226007, India e-mail: [email protected] ABSTRACT: A sequence stratigraphic study of terrigenous and carbonate rocks GEOLOGICAL FRAMEWORK of the Infra Krol Formation and Krol Group in the Lesser Himalaya fold and thrust belt of northern India was undertaken as part of a broader investigation The Infra Krol Formation and Krol Group are part of a Neoproterozoic and Lower of the signi®cance of carbon isotope data in Neoproterozoic successions. Eight Cambrian succession more than 12 km thick, cropping out in the Lesser Himalaya regional stratigraphic discontinuities were traced over a distance of nearly 300 in a series of doubly plunging synclines between Solan in the northwest and Nainital, km, and interpretations were anchored in a series of local studies involving the 280 km to the southeast (Fig. 1; Bhargava 1979; Shanker et al. 1989; Shanker et mapping of key beds and the measurement of closely spaced sections. Three of al. 1993; Shanker et al. 1997; Shanker and Mathur 1992). -
Metamorphism
Title page INTRODUCING METAMORPHISM Ian Sanders DUNEDIN EDINBURGH LONDON Contents Contents v Preface ix Acknowledgements x 1 Introduction 1 1.1 What is metamorphism? 1 1.1.1 Protoliths 1 1.1.2 Changes to the minerals 1 1.1.3 Changes to the texture 3 1.1.4 Naming metamorphic rocks 3 1.2 Metamorphic rocks – made under mountains 3 1.2.1 Mountain building 3 1.2.2 Directed stress, pressure and temperature in a mountain’s roots 4 1.2.3 Exhumation of a mountain’s roots 6 1.3 Metamorphism in local settings 6 1.3.1 Contact metamorphism 7 1.3.2 Hydrothermal metamorphism 7 1.3.3 Dynamic metamorphism 9 1.3.4 Shock metamorphism 9 2 The petrography of metamorphic rocks 11 2.1 Quartzite and metapsammite 11 2.1.1 Quartzite 11 2.1.2 Metapsammite 13 2.2 Metapelite 13 2.2.1 Slate 14 2.2.2 Phyllite and low-grade schist 16 2.2.3 Minerals and textures of medium-grade schist 17 2.2.4 The regional distribution of minerals in low- and medium-grade schist 20 2.2.5 Pelitic gneiss and migmatite 22 2.2.6 Metapelite in a contact aureole 23 2.2.7 The significance of Al2SiO5 for inferring metamorphic conditions 23 2.3 Marble 24 2.3.1 Pure calcite marble 24 2.3.2 Impure marble 26 2.3.3 Metasediments with mixed compositions 29 CONTENTS 2.4 Metabasite 30 2.4.1 Six kinds of metabasite from regional metamorphic belts 31 2.4.2 The ACF triangle for minerals in metabasites 36 2.4.3 P–T stability of metabasites, and metamorphic facies 38 vi 2.4.4 A metabasite made by contact metamorphism 40 2.5 Metagranite 41 2.5.1 Granitic gneiss and orthogneiss 41 2.5.2 Dynamic metamorphism -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
The Lithology, Geochemistry, and Metamorphic Gradation of the Crystalline Basement of the Cheb (Eger) Tertiary Basin, Saxothuringian Unit
Bulletin of Geosciences, Vol. 79, No. 1, 41–52, 2004 © Czech Geological Survey, ISSN 1214-1119 The lithology, geochemistry, and metamorphic gradation of the crystalline basement of the Cheb (Eger) Tertiary Basin, Saxothuringian Unit Jiří Fiala – Zdeněk Vejnar Academy of Sciences of the Czech Republic, Institute of Geology, Rozvojová 135, 165 00 Praha 6, Czech Republic. E-mail: [email protected] Abstract. The crystalline basement of the Cheb Tertiary Basin is comprised of muscovite granite of the Smrčiny Pluton and crystalline schists of the Saxothuringian Unit. With increasing depth (as seen from the 1190 m deep drill hole HV-18) this crystalline schist exhibits rapid metamorphic gradation, with the characteristic development of garnet, staurolite, and andalusite zones of subhorizontal arrangement. The dynamic MP-MT and static LP-MT crystallization phases were followed by local retrograde metamorphism. The moderately dipping to subhorizontal S2 foliation, which predominates in the homogeneous segments, is followed by subvertical S3 cleavage. The vertical succession of psammo-pelitic, carbonitic, and volcanogenic rock sequences, together with geochemical data from the metabasites, indi- cates a rock complex representing an extensional, passive continental margin setting, which probably originated in the Late Cambrian to Early Ordovi- cian. On the contrary, the geochemistry of the silicic igneous rocks and of the limestone non-carbonate components point to the compressional settingofa continental island arc. This disparity can be partly explained by the inheritance of geochemical characteristics from Late Proterozoic rocks in the source region. Key words: crystalline basement, Cheb Tertiary Basin, Saxothuringian, lithology, geochemistry, metamorphism Introduction formed by two-mica and muscovite granites from the younger intrusive phase of the Smrčiny Pluton (Vejnar The Cheb Tertiary Basin is considered to be a westernmost 1960). -
PRELIMINARY EVALUATION of BEDROCK POTENTIAL for NATURALLY OCCURRING ASBESTOS in ALASKA by Diana N
Alaska Division of Geological & Geophysical Surveys MISCELLANEOUS PUBLICATION 157 PRELIMINARY EVALUATION OF BEDROCK POTENTIAL FOR NATURALLY OCCURRING ASBESTOS IN ALASKA by Diana N. Solie and Jennifer E. Athey Tremolite (UAMES 34960) displaying the soft, friable fibers of asbestiform minerals. Sample collected from the Cosmos Hills area, Kobuk District, Alaska, by Eskil Anderson. Image courtesy of the University of Alaska Museum Earth Sciences Department. June 2015 Released by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Division of Geological & Geophysical Surveys 3354 College Road, Fairbanks, Alaska 99709-3707 907-451-5020 dggs.alaska.gov [email protected] $2.00 (text only) $13.00 (per map sheet) TABLE OF CONTENTS Abstract ................................................................................................................................................................................................................................. 1 Introduction ........................................................................................................................................................................................................................ 1 General geology of asbestos ......................................................................................................................................................................................... 2 Naturally occurring asbestos potential in Alaska .............................................................................................................................................. -
Categories of Information That Go in Each of the Lithology Tables
Oregon Geologic Digital Compilation Keywords for lithology table(s) data entry—revised 2/1/05, 1/1/06 Lithology mineral and composition table Alteration, to (mineral) includes weathering Blebs, composition Blocks, composition Cavity fill, composition Cavity lining, composition Cementation, composition Clasts, composition Clots, composition Concretions, composition Debris, composition Encrustation, composition Enrichment, composition Facies, composition Fiamme, composition Fossiliferous (general fossil types, not individual genus and species) Fracture fill, composition Fragments composition Grains, composition Impurities, composition Inclusions, composition Joint fill, composition Knobs, composition Lapilli, composition Layering, composition Luster, composition Matrix, composition Mineralogy (list of main minerals or lithologies) Mineralization (list of commodity minerals) Nodules, composition Oxidation, composition Particles, composition Partings, composition Patches, composition Phenocrysts, composition Purity, amount of or type Recrystallization, mineral Schlieren, composition Seams, composition of mineral fill Shards, composition Soil, composition Staining, composition Stringers, composition of mineral fill Veins (or veinlets), compositon of mineral/lithology fill Vesicle fill, composition Xenoliths, composition Zones, composition Lithology color table Fresh Weathered Staining (color only) Lithology major structures table—amounts of outcrop level characteristics (keyword is followed by a describing adjective or, if no adjective, is -
Geology of the Eoarchean, >3.95 Ga, Nulliak Supracrustal
ÔØ ÅÒÙ×Ö ÔØ Geology of the Eoarchean, > 3.95 Ga, Nulliak supracrustal rocks in the Saglek Block, northern Labrador, Canada: The oldest geological evidence for plate tectonics Tsuyoshi Komiya, Shinji Yamamoto, Shogo Aoki, Yusuke Sawaki, Akira Ishikawa, Takayuki Tashiro, Keiko Koshida, Masanori Shimojo, Kazumasa Aoki, Kenneth D. Collerson PII: S0040-1951(15)00269-3 DOI: doi: 10.1016/j.tecto.2015.05.003 Reference: TECTO 126618 To appear in: Tectonophysics Received date: 30 December 2014 Revised date: 30 April 2015 Accepted date: 17 May 2015 Please cite this article as: Komiya, Tsuyoshi, Yamamoto, Shinji, Aoki, Shogo, Sawaki, Yusuke, Ishikawa, Akira, Tashiro, Takayuki, Koshida, Keiko, Shimojo, Masanori, Aoki, Kazumasa, Collerson, Kenneth D., Geology of the Eoarchean, > 3.95 Ga, Nulliak supracrustal rocks in the Saglek Block, northern Labrador, Canada: The oldest geological evidence for plate tectonics, Tectonophysics (2015), doi: 10.1016/j.tecto.2015.05.003 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Geology of the Eoarchean, >3.95 Ga, Nulliak supracrustal rocks in the Saglek Block, northern Labrador, Canada: The oldest geological evidence for plate tectonics Tsuyoshi Komiya1*, Shinji Yamamoto1, Shogo Aoki1, Yusuke Sawaki2, Akira Ishikawa1, Takayuki Tashiro1, Keiko Koshida1, Masanori Shimojo1, Kazumasa Aoki1 and Kenneth D. -
Oregon Geologic Digital Compilation Rules for Lithology Merge Information Entry
State of Oregon Department of Geology and Mineral Industries Vicki S. McConnell, State Geologist OREGON GEOLOGIC DIGITAL COMPILATION RULES FOR LITHOLOGY MERGE INFORMATION ENTRY G E O L O G Y F A N O D T N M I E N M E T R R A A L P I E N D D U N S O T G R E I R E S O 1937 2006 Revisions: Feburary 2, 2005 January 1, 2006 NOTICE The Oregon Department of Geology and Mineral Industries is publishing this paper because the infor- mation furthers the mission of the Department. To facilitate timely distribution of the information, this report is published as received from the authors and has not been edited to our usual standards. Oregon Department of Geology and Mineral Industries Oregon Geologic Digital Compilation Published in conformance with ORS 516.030 For copies of this publication or other information about Oregon’s geology and natural resources, contact: Nature of the Northwest Information Center 800 NE Oregon Street #5 Portland, Oregon 97232 (971) 673-1555 http://www.naturenw.org Oregon Department of Geology and Mineral Industries - Oregon Geologic Digital Compilation i RULES FOR LITHOLOGY MERGE INFORMATION ENTRY The lithology merge unit contains 5 parts, separated by periods: Major characteristic.Lithology.Layering.Crystals/Grains.Engineering Lithology Merge Unit label (Lith_Mrg_U field in GIS polygon file): major_characteristic.LITHOLOGY.Layering.Crystals/Grains.Engineering major characteristic - lower case, places the unit into a general category .LITHOLOGY - in upper case, generally the compositional/common chemical lithologic name(s) -
A Data-Driven Approach for Lithology Identification Based on Parameter
energies Article A Data-Driven Approach for Lithology Identification Based on Parameter-Optimized Ensemble Learning Zhixue Sun 1, Baosheng Jiang 1,* , Xiangling Li 2, Jikang Li 1 and Kang Xiao 2 1 School of Petroleum Engineering, China University of Petroleum (East China), Qingdao 266580, China; [email protected] (Z.S.); [email protected] (J.L.) 2 PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China; [email protected] (X.L.); [email protected] (K.X.) * Correspondence: [email protected] Received: 19 June 2020; Accepted: 27 July 2020; Published: 30 July 2020 Abstract: The identification of underground formation lithology can serve as a basis for petroleum exploration and development. This study integrates Extreme Gradient Boosting (XGBoost) with Bayesian Optimization (BO) for formation lithology identification and comprehensively evaluated the performance of the proposed classifier based on the metrics of the confusion matrix, precision, recall, F1-score and the area under the receiver operating characteristic curve (AUC). The data of this study are derived from Daniudui gas field and the Hangjinqi gas field, which includes 2153 samples with known lithology facies class with each sample having seven measured properties (well log curves), and corresponding depth. The results show that BO significantly improves parameter optimization efficiency. The AUC values of the test sets of the two gas fields are 0.968 and 0.987, respectively, indicating that the proposed method has very high generalization performance. Additionally, we compare the proposed algorithm with Gradient Tree Boosting-Differential Evolution (GTB-DE) using the same dataset. The results demonstrated that the average of precision, recall and F1 score of the proposed method are respectively 4.85%, 5.7%, 3.25% greater than GTB-ED. -
A Systematic Nomenclature for Metamorphic Rocks
A systematic nomenclature for metamorphic rocks: 1. HOW TO NAME A METAMORPHIC ROCK Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: Web version 1/4/04. Rolf Schmid1, Douglas Fettes2, Ben Harte3, Eleutheria Davis4, Jacqueline Desmons5, Hans- Joachim Meyer-Marsilius† and Jaakko Siivola6 1 Institut für Mineralogie und Petrographie, ETH-Centre, CH-8092, Zürich, Switzerland, [email protected] 2 British Geological Survey, Murchison House, West Mains Road, Edinburgh, United Kingdom, [email protected] 3 Grant Institute of Geology, Edinburgh, United Kingdom, [email protected] 4 Patission 339A, 11144 Athens, Greece 5 3, rue de Houdemont 54500, Vandoeuvre-lès-Nancy, France, [email protected] 6 Tasakalliontie 12c, 02760 Espoo, Finland ABSTRACT The usage of some common terms in metamorphic petrology has developed differently in different countries and a range of specialised rock names have been applied locally. The Subcommission on the Systematics of Metamorphic Rocks (SCMR) aims to provide systematic schemes for terminology and rock definitions that are widely acceptable and suitable for international use. This first paper explains the basic classification scheme for common metamorphic rocks proposed by the SCMR, and lays out the general principles which were used by the SCMR when defining terms for metamorphic rocks, their features, conditions of formation and processes. Subsequent papers discuss and present more detailed terminology for particular metamorphic rock groups and processes. The SCMR recognises the very wide usage of some rock names (for example, amphibolite, marble, hornfels) and the existence of many name sets related to specific types of metamorphism (for example, high P/T rocks, migmatites, impactites). -
Stratigraphic Signature of the Late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and Inter- Regional Comparisons
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 2010 Stratigraphic signature of the late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and inter- regional comparisons Christopher R. Fielding University of Nebraska-Lincoln, [email protected] Tracy D. Frank University of Nebraska-Lincoln, [email protected] John L. Isbell University of Wisconsin-Milwaukee, [email protected] Lindsey C. Henry University of Wisconsin-Milwaukee Eugene W. Domack Hamilton College, Clinton, NY, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Fielding, Christopher R.; Frank, Tracy D.; Isbell, John L.; Henry, Lindsey C.; and Domack, Eugene W., "Stratigraphic signature of the late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and inter-regional comparisons" (2010). Papers in the Earth and Atmospheric Sciences. 263. https://digitalcommons.unl.edu/geosciencefacpub/263 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Published in Palaeogeography, Palaeoclimatology, Palaeoecology 298 (2010), pp. 70–90; doi:10.1016/j.palaeo.2010.05.023 Copyright © 2010 Elsevier B.V. Used by permission Submitted September 25, 2009; revised April 20, 2010; accepted May 20, 2010; published online June 1, 2010. Stratigraphic signature of the late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and inter-regional comparisons Christopher R.