DOCSLIB.ORG

Pattern Chart Pattern from a Custom-Designed Patternset

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Pattern Chart Pattern from a Custom-Designed Patternset EXPLANATION FGDC Digital Cartographic Standard for Geologic Map Symbolization Pattern number shown below box. Abbreviations: K, black; C, cyan; M, magenta; DO, dropout; R, red; B, brown. FGDC Document Number FGDC-STD-013-2006 Generic lookup-table number shown in upper left-hand corner of box. Number can be used to access a particular Pattern Chart pattern from a custom-designed patternset. For more specific information on these patterns, see discussion on p. A-38-1 of the "FGDC Digital Cartographic Standard for Geologic Map Symbolization" (available at http://ngmdb.usgs.gov/fgdc_gds/). [Pattern number below pattern box; generic lookup-table symbol number in upper left-hand corner of pattern box] Pattern Chart For guidelines on selecting patterns, see Section 5, entitled "Guidelines for Map Color and Pattern Selection," in the introductory text of the FGDC standards document. Digital files available at http://ngmdb.usgs.gov/fgdc_gds/ SURFICIAL PATTERNS (Series 100) SEDIMENTARY PATTERNS (Series 200) 101 102 103 104 130 131 132 133 161 162 163 164 201 202 203 204 225 226 227 228 250 251 252 253 101-K 101-C 101-M 101-DO 116-K 116-C 116-M 116-DO 123-K 123-C 123-M 123-DO 201-K 201-C 201-M 201-DO 215-K 215-C 215-M 215-DO 228-K 228-C 228-M 228-DO 105 106 107 108 109 134 135 136 137 138 165 166 167 168 205 206 207 208 229 230 231 232 254 255 256 257 258 102-K 102-C 102-M 102-R 102-DO 117-K 117-C 117-M 117-R 117-DO 124-K 124-C 124-M 124-DO 202-K 202-C 202-M 202-DO 216-K 216-C 216-M 216-DO 229-K 229-C 229-M 229-R 229-DO 110 111 112 113 139 140 141 142 169 170 171 172 173 209 210 211 212 233 234 235 236 259 260 261 262 103-K 103-C 103-M 103-DO 118-K 118-C 118-M 118-DO 132-K 132-C132-M 132-B 132-DO 204-K 204-C 204-M 204-DO 217-K 217-C 217-M 217-DO 230-K 230-C 230-M 230-DO 114 115 116 117 143 144 145 146 147 174 175 176 177 178 213 214 215 216 237 238 239 240 263 264 265 266 104-K 104-C 104-M 104-DO 119-K 119-C 119-M 119-R 119-DO 134-K 134-C 134-M 134-R 134-DO 206-K 206-C 206-M 206-DO 218-K 218-C 218-M 218-DO 231-K 231-C 231-M 231-DO 118 119 120 121 148 149 150 151 179 180 181 182 183 217 218 219 220 241 242 243 244 267 268 269 270 271 105-K 105-C 105-M 105-DO 120-K 120-C 120-M 120-DO 135-K 135-C 135-M 135-B 135-DO 207-K 207-C 207-M 207-DO 219-K 219-C 219-M 219-DO 232-K 232-C 232-M 232-B 232-DO 122 123 124 125 152 153 154 155 156 184 185 186 187 188 221 222 223 224 245 246 247 248 249 272 273 274 275 106-K 106-C 106-M 106-DO 121-K 121-C 121-M 121-R 121-DO 136-K 136-C 136-M 136-R 136-DO 214-K 214-C 214-M 214-DO 226-K 226-C 226-M 226-R 226-DO 233-K 233-C 233-M 233-DO 126 127 128 129 157 158 159 160 189 190 191 192 193 114-K 114-C 114-M 114-DO 122-K 122-C 122-M 122-DO 137-K 137-C 137-M 137-R 137-DO IGNEOUS PATTERNS (Series 300) MISCELLANEOUS AND METAMORPHIC PATTERNS (Series 400) 301 302 303 304 325 326 327 328 350 351 352 353 401 402 403 404 439 440 441 442 467 468 469 470 301-K 301-C 301-M 301-DO 313-K 313-C 313-M 313-DO 319-K 319-C 319-M 319-DO 401-K 401-C 401-M 401-DO 418-K 418-C 418-M 418-DO 430-K 430-C 430-M 430-DO 305 306 307 308 329 330 331 332 354 355 356 357 358 405 406 407 408 443 444 445 446 447 471 472 473 474 302-K 302-C 302-M 302-DO 314-K 314-C 314-M 314-DO 327-K 327-C 327-M 327-R 327-DO 402-K 402-C 402-M 402-DO 419-K 419-C 419-M 419-R 419-DO 431-K 431-C 431-M 431-DO 309 310 311 312 333 334 335 336 359 360 361 362 363 409 410 411 412 448 449 475 476 477 478 303-K 303-C 303-M 303-DO 315-K 315-C 315-M 315-DO 328-K 328-C 328-M 328-R 328-DO 403-K 403-C 403-M 403-DO 420-K 420-C 432-K 432-C 432-M 432-DO 313 314 315 316 337 338 339 340 364 365 366 367 413 414 415 416 417 450 451 479 480 481 482 304-K 304-C 304-M 304-DO 316-K 316-C 316-M 316-DO 330-K 330-C 330-M 330-DO 405-K 405-C 405-M 405-R 405-DO 423-K 423-C 433-K 433-C 433-M 433-DO 317 318 319 320 341 342 343 344 345 368 369 370 371 418 419 420 421 422 452 453 483 484 485 486 487 305-K 305-C 305-M 305-DO 317-K 317-C 317-M 317-R 317-DO 331-K 331-C 331-M 331-DO 406-K 406-C 406-M 406-R 406-DO 424-K 424-C 434-K 434-C 434-M 434-R 434-DO 321 322 323 324 346 347 348 349 423 424 425 426 454 488 489 490 491 492 306-K 306-C 306-M 306-DO 318-K 318-C 318-M 318-DO 411-K 411-C 411-M 411-DO 426 435-K 435-C 435-M 435-R 435-DO 427 428 429 430 455 456 493 494 495 496 497 412-K 412-C 412-M 412-DO 427-K 427-R 436-K 436-C 436-M 436-R 436-DO 431 432 433 434 457 458 459 460 461 416-K 416-C 416-M 416-DO 428-K 428-C 428-M 428-R 428-DO 435 436 437 438 462 463 464 465 466 417-K 417-C 417-M 417-DO 429-K 429-C 429-M 429-R 429-DO SEDIMENTARY LITHOLOGY PATTERNS (Series 600) METAMORPHIC, IGNEOUS, AND VEIN-MATTER LITHOLOGY PATTERNS (Series 700) GLACIAL AND PERIGLACIAL PATTERNS (Series 500) [Usually reserved for use on stratigraphic columns, sections, or charts] [Usually reserved for use on stratigraphic columns, sections, or charts] Glacial patterns (521–524) 601 602 603 605 606 607 608 645 646 647 648 649 650 651 Metamorphic lithology patterns (701–710) 530 531 534 535 536 701 702 703 704 705 706 601 602 603 605 606 607 608 645 646 647 648 649 650 651 Gravel or Gravel or Crossbedded gravel Breccia (1st option) Breccia (2nd option) Massive sand or Bedded sand or Sandy dolostone Silty dolostone Argillaceous or Cherty dolostone Bedded chert Bedded chert Fossiliferous conglomerate conglomerate or conglomerate sandstone sandstone or dolomite or dolomite shaly dolostone or dolomite (1st option) (2nd option) bedded chert (1st option) (2nd option) or dolomite 701 702 703 704 705 706 521-K 521-C 523-K 523-C 523-DO Metamorphism Quartzite Slate Schistose or Schist Contorted schist gneissoid granite 532 533 537 538 609 610 611 612 613 614 616 652 653 654 655 656 657 658 707 708 709 710 609 610 611 612 613 614 616 652 653 654 655 656 657 658 Crossbedded sand Crossbedded sand Ripple-bedded sand Argillaceous or Calcareous Dolomitic Silt, siltstone, Fossiliferous rock Diatomaceous Subgraywacke Crossbedded Ripple-bedded Peat Coal 522-K 522-C 524-K 524-C or sandstone or sandstone or sandstone shaly sandstone sandstone sandstone or shaly silt rock subgraywacke subgraywacke (1st option) (2nd option) 707 708 709 710 Schist and gneiss Gneiss Contorted gneiss Soapstone, talc, or serpentinite 662 Periglacial patterns (591–595) 617 618 619 620 621 622 623 659 660 661 663 664 665 Igneous and vein-matter lithology patterns (711–33) 580 581 711 712 713 714 715 716 617 618 619 620 621 622 623 659 660 661 662 663 664 665 Calcareous Dolomitic Sandy or silty Clay or clay Cherty shale Dolomitic shale Calcareous shale Bony coal or Underclay Flint clay Bentonite Glauconite Limonite Siderite siltstone siltstone shale shale or marl impure coal 711 712 713 714 715 716 591-K 591-C 624 625 626 627 628 629 630 666 Tuffaceous rock Crystal tuff Devitrified Volcanic breccia Volcanic breccia Zeolitic rock 667 668 669 670 671 672 tuff and tuff or agglomerate 582 583 717 718 719 720 721 722 624 625 626 627 628 629 630 666 667 668 669 670 671 672 Carbonaceous Oil shale Chalk Limestone Clastic Fossiliferous clastic Nodular or irregularly Phosphatic-nodular Gypsum Salt Interbedded Interbedded Interbedded ripple- Interbedded shale shale limestone limestone bedded limestone rock sandstone and sandstone and bedded sandstone and silty limestone siltstone shale and shale (shale dominant) 592-K 592-C 717 718 719 720 721 722 631 632 633 634 635 636 637 673 674 675 676 677 678 679 Basaltic flows Granite (1st option) Granite (2nd option) Banded Igneous rock Igneous rock 584 585 igneous rock (1st option) (2nd option) 723 724 725 726 727 728 631 632 633 634 635 636 637 673 674 675 676 677 678 679 Limestone, irregular Crossbedded Cherty crossbedded Cherty and sandy Oolitic Sandy limestone Silty limestone Interbedded shale Interbedded shale Interbedded calc- Interbedded Interbedded Interbedded Interbedded 593-K 593-C (burrow?) fillings of limestone limestone crossbedded limestone and limestone and limestone areous shale and silty limestone limestone and limestone and limestone and shale saccharoidal dolomite clastic limestone (shale dominant) (shale dominant) limestone (shale and shale shale (1st option) shale (2nd option) (limestone dominant) (1st option) (2nd option) dominant) 723 724 725 726 727 728 586 587 638 639 640 641 642 643 644 680 681 682 683 684 685 686 Igneous rock Igneous rock Igneous rock Igneous rock Igneous rock Igneous rock (3rd option) (4th option) (5th option) (6th option) (7th option) (8th option) 729 730 731 732 733 638 639 640 641 642 643 644 680 681 682 683 684 685 686 594-K 594-C Argillaceous or Cherty limestone Cherty limestone Dolomitic limestone, Dolostone or Crossbedded Oolitic dolostone Interbedded Till or diamicton Till or diamicton Till or diamicton Loess (1st option) Loess (2nd option) Loess (3rd option) shaly limestone (1st option) (2nd option) limy dolostone, or dolomite dolostone or or dolomite limestone and (1st option) (2nd option) (3rd option) 588 589 limy dolomite dolomite calcareous shale 729 730 731 732 733 Porphyritic rock Porphyritic rock Vitrophyre Quartz Ore (1st option) (2nd option) 595-K 595-C.
Load more

Recommended publications
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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)
    [Show full text]
  • 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.
    [Show full text]
  • High-Resolution Stratigraphy and Lithology of an Outcrop Within the Grundy Formation (Pennsylvanian), Harlan County, Southeast Kentucky
    Eastern Kentucky University Encompass Geosciences Undergraduate Theses Geosciences Spring 5-2020 High-resolution Stratigraphy and Lithology of an Outcrop within the Grundy Formation (Pennsylvanian), Harlan County, Southeast Kentucky Andrew Hensley Eastern Kentucky University Follow this and additional works at: https://encompass.eku.edu/geo_undergradtheses Recommended Citation Hensley, Andrew, "High-resolution Stratigraphy and Lithology of an Outcrop within the Grundy Formation (Pennsylvanian), Harlan County, Southeast Kentucky" (2020). Geosciences Undergraduate Theses. 7. https://encompass.eku.edu/geo_undergradtheses/7 This Restricted Access Thesis is brought to you for free and open access by the Geosciences at Encompass. It has been accepted for inclusion in Geosciences Undergraduate Theses by an authorized administrator of Encompass. For more information, please contact [email protected]. High-resolution Stratigraphy and Lithology of an Outcrop within the Grundy Formation (Pennsylvanian), Harlan County, Southeast Kentucky By Andrew Hensley Submitted to Walter S. Borowski Senior Thesis (GLY 499) May 2020 i TABLE OF CONTENTS Abstract……………………………………………………………………………………… 1 Introduction………………………………………………………………………….…….... 2 Methods……………………………………………………………………………………... 2 Results………………………………………………………………………………………..3 Coarsening-upward Sequence 1…………………..…………………………………5 Coarsening-upward Sequence 2…………………..…………………………………7 Coarsening-upward Sequence 3…………………..…………………………………9 Coarsening-upward Sequence 4…………………………………………………….11 Coarsening-upward Sequence
    [Show full text]
  • Rocks and Minerals) in the Open Wordnet for English
    Proceedings of the Workshop on Multimodal Wordnets (MMWN-2020), pages 33–38 Language Resources and Evaluation Conference (LREC 2020), Marseille, 11–16 May 2020 c European Language Resources Association (ELRA), licensed under CC-BY-NC Inclusion of Lithological terms (rocks and minerals) in The Open Wordnet for English Alexandre Tessarollo, Alexandre Rademaker Petrobras, IBM Research and FGV/EMAp [email protected], [email protected] Abstract We extend the Open WordNet for English (OWN-EN) with rock-related and other lithological terms using the authoritative source of GBA’s Thesaurus. Our aim is to improve WordNet to better function within Oil & Gas domain, particularly geoscience texts. We use a three step approach: a proof of concept-level extension of WordNet, a major extension on which we evaluate the impact with positive results and a full extension encompassing all GBA’s lithological terms. We also build a mapping to GBA which also links to several other resources: WikiData, British Geological Survey, Inspire, GeoSciML and DBpedia. Keywords: wordnet, rocks, lithology, domain extension, geology, NLP 1. Introduction 2012). WordNet extensions for specific domains are rela- tively common. Oil & Gas Exploration and Production companies annu- Medical WordNet (MWN) (Smith and Fellbaum, 2004) re- ally invest billions of dollars gathering documents such views PWN medical terms through a corpus which includes as reports, scientific articles, business intelligence articles a validated corpus of sentences involving specific medically and so on. These documents are the main base for ma- relevant vocabulary. The corpus is composed by the defini- jor decisions such as whether to drill exploratory wells, bid tions of medical terms already existing in WordNet, sen- or buy, production schedules and risk assessments (Rade- tences generated via the semantic relations in PWN and maker, 2018).
    [Show full text]
  • Characteristics of Log Responses and Lithology Determination of Igneous Rock Reservoirs
    NANJING INSTITUTE OF GEOPHYSICAL PROSPECTING AND INSTITUTE OF PHYSICS PUBLISHING JOURNAL OF GEOPHYSICS AND ENGINEERING J. Geophys. Eng. 1 (2004) 51–55 PII: S1742-2132(04)73730-9 Characteristics of log responses and lithology determination of igneous rock reservoirs Buzhou Huang and Baozhi Pan School of Geoexploration Science and Technology, Jilin University, Changchun 130026, China E-mail: [email protected] Downloaded from https://academic.oup.com/jge/article/1/1/51/5127508 by guest on 02 October 2021 Received 1 August 2003 Accepted for publication 1 November 2003 Published 16 February 2004 Online at stacks.iop.org/JGE/1/51 (DOI: 10.1088/1742-2132/1/1/006) Abstract The determination of the lithology of deep igneous rocks in the northern Songliao Basin in China has been found to be difficult because of insufficient core-analysis data and accurate descriptions of cuttings in the area. This paper presents a method for determining the lithology of these rocks. First, the igneous rocks are divided into six classes according to cores and cuttings in the area. Then, for each class, a statistical analysis is performed for 11 log data sets to determine their log characteristics. Finally, the different lithologies of the igneous rock reservoirs in the area are automatically determined using the maximum membership function rule of fuzzy mathematics. A comparison between the results obtained and the lithologic column obtained from cores or cuttings shows that this method gives good results for the determination of igneous rock lithology in the area. Keywords: lithology determination, igneous rocks, log characteristics, maximum membership function 1.
    [Show full text]
  • Geology of the Nuvvuagittuq Belt
    Earth’s Oldest Rocks Edited by Martin J. van Kranendonk, R. Hugh Smithies and Vickie C. Bennett Developments in Precambrian Geology, Vol. 15 (K.C. Condie, Series Editor) ©2007 Elsevier B.V. All rights reserved. THE GEOLOGY OF THE 3.8 GA NUVVUAGITTUQ (PORPOISE COVE) GREENSTONE BELT, NORTHEASTERN SUPERIOR PROVINCE, CANADA. Jonathan O’Neil1, Charles Maurice2, Ross K. Stevenson3,4, Jeff Larocque5, Christophe Cloquet6, Jean David3 & Don Francis1 1 Earth & Planetary Sciences, McGill University and GÉOTOP-UQÀM-McGill, 3450 University St. Montreal, QC, Canada, H3A 2A7 ([email protected]) 2 Bureau de l’exploration géologique du Québec, Ministère des Ressources naturelles et de la Faune, 400 boul. Lamaque Val d’Or, QC, J9P 3L4 3 GÉOTOP-UQÀM-McGill, Université du Québec à Montréal, C.P. 8888, succ. centre-ville, Montreal, QC, Canada H3C 3P8 4 Département des Sciences de la Terre et de l’Atmosphère, Université du Québec à Montréal, C.P. 8888, succ. centre-ville Montreal, QC, Canada H3C 3P8 5 School of Earth and Oceanic Sciences, University of Victoria, P.O. Box 3055 STN CSC, Victoria, BC, Canada, V8W 3P6 6 INW-UGent, Department of analytical chemistry, Proeftuinstraat 86, 9000 GENT, Belgium Abstract The Nuvvuagittuq greenstone belt is a 3.8 Ga supracrustal succession preserved as a raft in remobilised tonalities along the eastern coast of Hudson Bay. The dominant lithology of the belt is a quartz-ribboned grey amphibolite composed of variable proportions of cummingtonite, biotite and plagioclase. Although the amphibolites have mafic compositions, the presence of cummingtonite rather than hornblende in these rocks reflects their low Ca contents, which may result from the alteration and metamorphism of mafic pyroclastic rocks.
    [Show full text]
  • Geochemistry of the Boring Lava Along the West Side of the Tualatin Mountains and of Sediments from Drill Holes in the Portland and Tualatin Basins, Portland, Oregon
    Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 10-6-1995 Geochemistry of the Boring Lava along the West Side of the Tualatin Mountains and of Sediments from Drill Holes in the Portland and Tualatin Basins, Portland, Oregon Michelle Lynn Barnes Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons Let us know how access to this document benefits ou.y Recommended Citation Barnes, Michelle Lynn, "Geochemistry of the Boring Lava along the West Side of the Tualatin Mountains and of Sediments from Drill Holes in the Portland and Tualatin Basins, Portland, Oregon" (1995). Dissertations and Theses. Paper 4990. https://doi.org/10.15760/etd.6866 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. THESIS APPROVAL The abstract and thesis of Michelle Lynn Barnes for the Master of Science in Geology were presented October 6, 1995, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: Tre"'\7'6r D. Smith Representative of the Office of Graduate Studies DEPARTMENT APPROVAL: .~arvin H. Beeson, Chair ( Department of Geology * * * * * * * * * * * * * * * * * * * * * * * * * * * * * ACCEPTED FOR PORTLAND STATE UNIVERSITY BY THE LIBRARY ... /}7 / '} . ,_ c.:·· by on ,::x / •.c:..14,.g..vd&&.· /9 ~5" ABSTRACT An abstract of the thesis of Michelle Lynn Barnes for the Master of Science in Geology presented October 6, 1995. Title: Geochemistry of the Boring Lava along the West Side of the Tualatin Mountains and of Sediments from Drill Holes in the Portland and Tualatin Basins, Portland, Oregon.
    [Show full text]