Back Matter (PDF)

Total Page:16

File Type:pdf, Size:1020Kb

Back Matter (PDF) Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. Abadeh Section (Iran) 74, 81, 83, 112 Annweiler Formation 397 Abadehceras 198 Anomalonema reumauxi–Peudestheria simoni assemblage Abichites 199 zone 370, 372–373 Abo Formation 73, 408, 409, 412, 425 Antarctica, palynostratigraphy 337 Abrahamskraal Formation 64, 78, 80, 418, 428 Anthracolithic System 25 radiometric dating 86 Anuites 193 Abrek Formation 295 Apache Dam Formation 409 acritarchs 322–323 Aquaw Creek (Colorado), magnetic polarity data 66 Admiral Formation 410 Arabia, palynostratigraphy 333, 333 Adrianites 194 Arabia Plate, fusuline biostratigraphy 255 A. elegans 195 Araksian Stage 40 Afghanistan Arasella 199 fusuline biostratigraphy 255, 260–261 Araxoceras spp. 196, 198 Agathiceras 187, 189 A. latissimum 198 Aidaralash CreekGSSP (Kazakstan)3, 28,29, 32, 53,67, 88,187,321,325 A. ventrosulcatum 198 Akiyoshi Terrane, fusuline biostratigraphy 270–271, 271 Archer City Formation 410, 411 Akmilleria 189 archosaurs 51 Aktastinian Substage 2, 33, 189 Argentina ammonoid assemblages 185 magnetic polarity data 64, 69, 72 Aktasty River Section 33 palynostratigraphy 330, 331, 331 Aktastynian Stage, ammonoid assemblages 185 tetrapods 387 Aktubinskia 189 Aricoceras 192 Aktyubinsk section 33 Aristoceras 187 Al Khlata Formation 336 Aristoceratoides 194 Alaska Region, fusuline biostratigraphy 255 Arizona, tetrapods 412–413 Albaillella cavitata interval zone 154, 157 Arnhardtia 39 Albaillella excelsa interval zone 155 Arrayo de Alamillo Formation 395, 409 Albaillella levis interval zone 155 Arroya del Agua Formation 408, 409, 425 Albaillella sinuata abindance zone 148–149 Arroya Formation 410 Albaillella triangularis interval zone 155, 157 Arroyo Vale Formation 411 Albaillella xiaodongensis assemblage zone 148 Artinskia spp. Albaillella yaoi abundance zone 155–156, 157 A. irinae 187, 189 Alibashites 199 A. kazakhstanica 187 Almites 187, 189 Artinskian Age, age calibration 52 Altudoceras 193, 196 Artinskian Stage 1, 2,33 Amana Formation 69 ammonoid assemblages 185 Amarassian Stage 40 ammonoid biostratigraphy 189–191, 191 ammonoid assemblages 185, 196 conodont biostratigraphy 120, 124, 126, 129, 130, 131 Amb Formation 309 first recognized 25 ammonoids 8–9, 30, 31,41–42 foraminiferal biostratigraphy 233 biostratigraphy fusuline chronostratigraphy 275 Cisuralian 187 fusuline genera 254 Artinskian 187–188 GSSP discussions 3, 33 Asselian 189–191 Perrinites zone 185 Kungurian 191–192 polarity data 63, 64, 66,68–69 Sakmarian 188–189 radiolaria zones 148 Guadalupian 192–193 rugose coral biostratigraphy Capitanian 195–197 Inner Mongolia–NE China and Japan 170 Roadina 193–194 South China and Indochina 166, 169 Wordian 194–195 87Sr/86Sr values 109, 113 Lopingian 197–198 volcanic ash beds 4 Changhsingian 199 Artioceras 189 Wuchiapingian 198 Artioceratoides 190 historical review 185, 187 Asitka Group 69 zones 186 Assel River Section 32 amniotes, diversification 51 Asselian Age, age calibration 52 amphibians Asselian Stage 1, 2, 32, 52–53 zonation 379, 415 ammonoid biostratigraphy 187–188, 188 see also tetrapods ammonoid assemblages 185 Amphisauropus 389, 389, 392, 393, 395 base first defined 28 Amushan Formation 294–295 conodont biozones 120, 122–128, 124, 126, 130 Anatsabites 194 first recognized 25 Andelosaurus 407 foraminiferal biostratigraphy 233 Anderssonoceras 198 fusuline chronostratigraphy 274, 275 Andrianovia 189 fusuline genera 254 Anfuceras 198 polarity data 63, 64, 65, 66,67–68 Angara radiolaria zones 147–148 Palaeokingdom 350, 355–356 rugose coral biostratigraphy palynostratigraphy 324, 327–329 Inner Mongolia–NE China and Japan 170 phytogeographic province 323–324, 324 South China and Indochina 166 Angjie Formation 304 87Sr/86Sr values 109, 113 Angrenoceras 197 volcanic ash beds 4 446 INDEX assemblage zones, role of 367 Russian Far East 294, 295–296 Assistance Formation 193, 194, 291 Palaeoequatorial Realm 299 astrochronology 57 China, South 296–298, 299 Atrasado Formation 380, 409 Iran, north 298–300, 299 Atsabites 190 Mediterranean 299, 300 Aulacogastrioceras 193 Texas, West 299, 300–301 Australia Transcaucasia 298–300, 299 brachiopod biostratigrapy, Southern Transitional Zone 302, 302 Eastern 306–308, 307 Baoshan Block 301–303, 302 Western 307, 308–309 Karakoram (Pakistan) 302, 305 first remanent magnetization study 61 Lhasa Block 302, 304 magnetic polarity data 76 Oman 302, 304–305 palynostratigraphy 334–335, 335, 337 Pamirs, SE 302, 305–306 tetrapods 387 Sibumasu Black 302, 303 Austria, tetrapods 387 South Qiangtang Block 302, 303–304 Autunia 39 Tengchong Block 301–303, 302 Autunia conferta Zone 350 Turkey 302, 304–305 Autunian Series 36,38–39 87Sr/86Sr values 109 Autunian Stage 350 Bransonoceras 190 Avushoceras 198 Branxton Formation 306 Brazil Baigendzhinian Stage 189 palynostratigraphy 330, 331 ammonoid assemblages 185 tetrapods 387, 406, 412, 415–416, 425, 427 Baigendzhinian Substage 2, 33, 190 Brevaxina dyhrenfurthi 38 Balfour Formation 84, 418 Broughton Formation 76, 307 Balic Formation 336 Buena Vista Formation 425 Bamyaniceras 190 Bulunites 188, 189 Baoqingian Substage 2,35 Bursum Formation 187, 379, 380, 408, 409, 412, 425 Baoshan Block Bursumian Substage 28, 39 brachiopod biostratigraphy 301–303, 302 foraminiferal biozonation 234 fusuline biostratigraphy 255, 264, 266 Burtsevian Substage 4, 34 Baraioceras 191 Byro Group 189, 190, 192 Batrachichnus 389, 389, 392, 393, 395 Bead Mountain Formation 410 Cache Creek Formation 195 Beaufort Group 57, 64, 78, 79, 80, 418, 427 Cache Creek Terrane, fusuline biostratigraphy 271, 272–273 Belcher Channel Formation 187 Callipteris–Comia–Iniopteris assemblage 356 Bell Canyon Formation 54, 301 Callipteris spp. Zone 351 Belle Plains Formation 410 Callytharra Formation 188, 302 Bellerophon Formation 300 Canada Berry Formation 307 brachiopod biostratigraphy, Western 290–291, 291 Biamiceras 192 fusuline biostratigraphy 255 Biarmian Series 73, 73–74, 423 tetrapods 387, 396 biochronological events 21, 405 see also North America and North American Craton biostratigraphic datums 21, 405 Cancellina 38 bivalve biostratigraphy 11, 15 Canfanggou Group 424 Blaine Formation 410, 412, 416, 417 Capitan Formation 34, 196 blattids 15 Capitanian Age, age calibration 52,54 Boesites 187, 188, 189 Capitanian Stage 2, 2, 27, 34, 36,39 Bolorian Stage 38, 38, 275, 276 ammonoid assemblages 185 fusuline genera 254 ammonoid biostratigraphy 195–197, 197 Boreal Realm, brachiopod biostratigraphy 290–293, 291 conodont biostratigraphy 120, 124, 126, 130, 133–134 Botrichiopsis Zone 354 foraminiferal biostratigraphy 234 Boyevaya Gora Section 75,81 fusuline chronostratigraphy 275 brachiopods fusuline genera 254 biostratigraphy 10, 41 GSSP 4, 54 diversity 289 magnetic polarity data 70, 76, 77, 90 life style 289 radiolaria zones 153–154 palaeobiogeography 289–290, 290 rugose coral biostratigraphy 169–170 Boreal Realm 291 87Sr/86Sr values 109, 111, 113, 114 Greenland 291–292, 291 Capitanian Substage, ammonoid assemblages 185 Siberian Plate 291, 292–293 carbon isotope stratigraphy 5–7 Spitsbergen 291–292, 291 carbon isotopic variation 165 Urals (Russia) 291, 293 Carboniferous–Permian boundary see Permo–Carboniferous Verkhoyansk Fold Belt 291, 292–293 Cardiella 187, 188, 189 Western Canada 290–291, 291 Carnic Alps, fusuline biostratigraphy 262, 263 Gondwanan Realm 306, 307 Carrandibby Formation 308 Australia, Western 307, 308–309 Casper Formation 72, 73 Australia, Eastern 306–308, 307 Castile Formation 39 Himalaya Tethys Zone 307, 309–310 Cathaysia India 307, 309–310 Palaeokingdom 350, 352–354 New Zealand 307, 308 palynostratigraphy 329 Pakistan, Salt Range 307, 309–310 phytogeographic province 323–324, 324 South America 307, 310 Cathaysiopteris whitei Zone 353 Northern Transitional Zone 294 Cathaysiopteris yochelsonii Zone 352 China 294–295, 294 Cathedral Mountain Formation 39, 192 Japan 294, 296 Cathedralian Substage 2, 39, 275 Mongolia, Inner 294–295, 294 first suggested 28 Mongolia, Southern 294, 295 foraminiferal biozonation 234 north Pamirs 296 Cedar Mesa Sandstone 412 INDEX 447 Central America, rugose coral biostratigraphy 174 Central America 174 Central Asian Ocean (CAO) 295, 296 Gondwana–Perigondwana 171–172 Cerro Carrizalito Formation 72 Inner Mongolia–NE China and Japan 170–171 Chainaha Formation 304 North America 174 Chambin Formation 195 South China and Indochina 166–169, 168 Chandalazian Regional Stage 196 Svalbard 173 Changhsing Formation 35, 297, 329 Ural Mountains 173 Changhsingian Age, age calibration 52 87Sr/86Sr values 113–114 Changhsingian Stage 2, 2, 35, 81 tetrapod chronology 407, 408–416, 423 ammonoid biostratigraphy 199 tetrapod tracks 387 conodont biostratigraphy 120, 124, 126, 130, 136–137 clam shrimps see conchostracans foraminiferal biostratigraphy 235 Clarkina fusuline chronostratigraphy 275 C. abadehensis 137 fusuline genera 254 C. asymmetrica Zone 135 GSSP 4 C. changxingensis Zone 35, 136 magnetic polarity data 70, 81, 83, 83 C. dukouensis Zone 135 radiolaria zones 155–156 C. giangyuanensis Zone 135 rugose coral biostratigraphy 170 C. hambastensis 136 87Sr/86Sr values 111, 112, 113 C. hongshuiensis 39 Changhsingoceras 194, 199 C. hongshuiensis Zone 134 charophytes 13 C. leveni Zone 135 Chekiangoceras 193 C. liangshanensis 135, 136 chemical abrasion thermal ionization mass spectrometry (CA-TIMS) C. longicispidata Zone 136 52, 55 C. meishanensis Zone 136–137 chemostratigraphy 43 C. nodosa 136 Cheremushka Section 75,78 C. orientalis Zone 135–136, 136 Cherry Canyon Formation 73 C. postbitteri Zone 4, 35, 55, 135 Chhidru
Recommended publications
  • Precise Age and Biostratigraphic Significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA
    Precise age and biostratigraphic significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA Spencer G. Lucas1, Bruce D. Allen2, Karl Krainer3, James Barrick4, Daniel Vachard5, Joerg W. Schneider6, William A. DiMichele7 and Arden R. Bashforth8 1New Mexico Museum of Natural History, 1801 Mountain Road N.W., Albuquerque, New Mexico, 87104, USA email: [email protected] 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, New Mexico, 87801, USA email: [email protected] 3Institute of Geology and Paleontology, University of Innsbruck, Innsbruck, A-6020, Austria email: [email protected] 4Department of Geosciences, Texas Tech University, Box 41053, Lubbock, Texas, 79409, USA email: [email protected] 5Université des Sciences et Technologies de Lille, UFR des Sciences de la Terre, UPRESA 8014 du CNRS, Laboratoire LP3, Bâtiment SN 5, F-59655 Villeneuve d’Ascq, Cédex, France email: [email protected] 6TU Bergakademie Freiberg, Cottastasse 2, D-09596 Freiberg, Germany email:[email protected] 7Department of Paleobiology, NMNH Smithsonian Institution, Washington, DC 20560 email: [email protected] 8Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark email: [email protected] ABSTRACT: The Kinney Brick Quarry is a world famous Late Pennsylvanian fossil Lagerstätte in central New Mexico, USA. The age assigned to the Kinney Brick Quarry (early-middle Virgilian) has long been based more on its inferred lithostratigraphic position than on biostratigraphic indicators at the quarry. We have developed three datasets —-stratigraphic position, fusulinids and conodonts— that in- dicate the Kinney Brick Quarry is older, of middle Missourian (Kasimovian) age.
    [Show full text]
  • Blue River Valley Stratigraphic Chart
    Blue River Valley Hydrogeologic Geologic Period Phase Stratigraphic Unit Unit Modern Alluvium and outwash deposits Alluvial Aquifer Quaternary Glacial deposits Glacial deposits Glaciation Older stream and outwash terrace Local perched deposits aquifer Troublesome Formation Local aquifer Neogene Extension Volcanic rocks Volcanics Paleogene Transition Paleogene and Cretaceous intrusive Crystalline rocks bedrock Laramide Pierre Shale Smoky Hill Member Fort Hayes Limestone Pierre confining Niobrara Niobrara Formation Cretaceous unit Interior Carlile Shale Seaway Greenhorn Limestone Graneros Shale Benton Group Dakota Sandstone Dakota Aquifer Morrison Formation Morrison Aquifer Jurassic Mesozoic Entrada Sandstone Entrada Aquifer Sandstones Chinle confining Triassic Chinle Formation unit Permian Maroon Formation Ancestral Maroon-Minturn Rocky Aquifer Mountains Minturn Formation Pennsylvanian Mississippian No strata Devonian Chaffee Group Paleozoic Silurian Mississippian- Carbonates Cambrian Ordovician Manitou Formation carbonate aquifer Dotsero Formation and Cambrian Sawatch Sandstone Crystalline rocks of igneous and Crystalline Precambrian Precambrian metamorphic origin in mountainous bedrock region Table 12a-05-01. Blue River Valley stratigraphic chart. Blue River Valley Unit Thickness Hydrogeologic Geologic Period Phase Stratigraphic Unit Physical Characteristics Hydrologic Characteristics (ft) Unit Well to poorly-sorted, uncemented sands, silts and gravels along modern Modern Alluvium and outwash deposits >35 Alluvial Aquifer streams and
    [Show full text]
  • Pennsylvanian Minturn Formation, Colorado, U.S.A
    Journal of Sedimentary Research, 2008, v. 78, 0–0 Research Articles DOI: 10.2110/jsr.2008.052 DEPOSITS FROM WAVE-INFLUENCED TURBIDITY CURRENTS: PENNSYLVANIAN MINTURN FORMATION, COLORADO, U.S.A. 1 2 2 3 2 M. P. LAMB, P. M. MYROW, C. LUKENS, K. HOUCK, AND J. STRAUSS 1Department of Earth & Planetary Science, University of California, Berkeley, California 94720, U.S.A. 2Department of Geology, Colorado College, Colorado Springs, Colorado 80903, U.S.A. 3Department of Geography and Environmental Sciences, University of Colorado, Denver, Colorado, 80217-3363 U.S.A. e-mail: [email protected] ABSTRACT: Turbidity currents generated nearshore have been suggested to be the source of some sandy marine event beds, but in most cases the evidence is circumstantial. Such flows must commonly travel through a field of oscillatory flow caused by wind-generated waves; little is known, however, about the interactions between waves and turbidity currents. We explore these interactions through detailed process-oriented sedimentological analysis of sandstone event beds from the Pennsylvanian Minturn Formation in north-central Colorado, U.S.A. The Minturn Formation exhibits a complex stratigraphic architecture of fan-delta deposits that developed in association with high topographic relief in a tectonically active setting. An , 20–35-m- thick, unconformity-bounded unit of prodelta deposits consists of dark green shale and turbidite-like sandstone beds with tool marks produced by abundant plant debris. Some of the sandstone event beds, most abundant at distal localities, contain reverse- to-normal grading and sequences of sedimentary structures that indicate deposition from waxing to waning flows. In contrast, proximal deposits, in some cases less than a kilometer away, contain abundant beds with evidence for deposition by wave- dominated combined flows, including large-scale hummocky cross-stratification (HCS).
    [Show full text]
  • Notes on the Mountain Limestone and Lower Carboniferous Rocks of the Fifeshire Coast from Burntisland to St Andrews
    ( 385 ) XVI.—Notes on the Mountain Limestone and Lower Carboniferous Rocks of the Fifeshire Coast from Burntisland to St Andrews. By the Rev. THOMAS BROWN, Edinburgh. (Read 17th April 1860.) Introduction. Mountain Limestone—continued. I. General Course of Strata. 2. Estuarine Strata, F to L. II. Trap Rocks. 3. Limestone L. III. Mountain Limestone. IV. Lower Carboniferous. 1. Six Upper Limestones, A to F. Myalina Beds. Corals. Petrified Trees. Shells. Marine Beds. Crustacea. Fossils. Fish. V. Results—The Two Groups defined. Tuberculated Fish. Introduction. In this paper I shall first refer to the circumstances under which the follow- ing observations were made. I had gone in the autumn of 1856 for a few weeks to Elie on the Fife coast, and was induced, as a means of relaxation and exercise in the open air, to pay some attention to the geology of the neighbourhood, resuming for a brief interval what was once a favourite pursuit. About a mile to the east of the village, I found a stratum well deserving attention—a thin bed of limestone—dipping in- land a little beyond the cliff on which stands the ruined Castle of Ardross. The fossil shells which it contained were of unusual form, and beautifully preserved ; there were fish remains of two or three species, and a small group of crustaceans still more remarkable. Among the fish I thought I could detect the large scales of an Irish species—the Holoirtijchius Fortlockii—and among the crustaceans there were the valves of Dithyrocaris, a genus particularly characteristic of the Irish beds. At once the question arose whether these fossils might not serve as links connecting this Ardross bed with the Irish series.
    [Show full text]
  • Wec01's SSSS Fossils Test 2019
    wec01’s SSSS Fossils Test 2019 Team Name: _________________KEY________________ Team Number: ___KEY___ Team Members: ____________KEY____________, ____________KEY____________ This test consists of 18 stations with a total of 200 points. Each answer is worth one point except where specified otherwise. You are only given 2 ½ minutes with the specimens at each station, however you can work on any station’s questions at any time. Scoring Station 1: ___10___ / 10 Station 10: ___12___ / 12 Station 2: ___10___ / 10 Station 11: ____9___ / 9 Station 3: ___11___ / 11 Station 12: ___11___ / 11 Station 4: ___10___ / 10 Station 13: ___10___ / 10 Station 5: ___10___ / 10 Station 14: ___10___ / 10 Station 6: ____9___ / 9 Station 15: ___12___ / 12 Station 7: ____9___ / 9 Station 16: ____9___ / 9 Station 8: ___10___ / 10 Station 17: ___10___ / 10 Station 9: ____9___ / 9 Station 18: ___29___ / 29 Total: __200___ / 200 Team Number: _KEY_ Station 1: Dinosaurs (10 pt) 1. Identify the genus of specimen A Tyrannosaurus (1 pt) 2. Identify the genus of specimen B Stegosaurus (1 pt) 3. Identify the genus of specimen C Allosaurus (1 pt) 4. Which specimen(s) (A, B, or C) are A, C (1 pt) Saurischians? 5. Which two specimens (A, B, or C) lived at B, C (1 pt) the same time? 6. Identify the genus of specimen D Velociraptor (1 pt) 7. Identify the genus of specimen E Coelophysis (1 pt) 8. Which specimen (D or E) is commonly E (1 pt) found in Ghost Ranch, New Mexico? 9. Which specimen (A, B, C, D, or E) would D (1 pt) specimen F have been found on? 10.
    [Show full text]
  • Prepared by the U.S. Geological Survey in Cooperation with Fort
    United States Department of the Interior Geological Survey Albuquerque, New Mexico Site study for a water well, Fort Wingate Army Ordnance Depot, McKinley County, New Mexico John W. Shomaker 1* Prepared by the U.S. Geological Survey in cooperation with Fort Wingate Army Ordnance Depot Open-file report April 1968 Contents Page — 4 Introduction — The stratigraphlc section in the Fort Wingate area Consideration of aquifers for a dependable water supply 17 _________ 22 Suggested well location y 25 Production well construction 27 Sutanary ~~ References cited Illustrations Reference page Figure l.-Map showing location of Fort Wingate Army Depot, and area of well-site investigation 4 2.—Altitude of the top of Glorleta Sandstone in Tidnlty of Headquarters area — ' (In"ocket) 3.—Depth to top of Precambrian granite and depth to top of Glorieta Sandstone in vicinity of Headquarters area — (I2 ■■• •■■ Site study for * water well, Fort Wlngate Army Ordnance Depot, McKinley County, New Mexico By John W. Shomaker Introduction Th« Fort Wingate Army Depot (fig. 1) is now supplied with water r . Figure 1 (caption on next page) belongs near here. from only one source, well No. 68 which is 1,125 feet deep. The well casing is deteriorating and the well nay fail. The Depot considers this an emergency situation that requires a new well to be drilled as soon as possible. In addition, the Army Materiel Command has suggested to the Depot that the total ground-water resources of the Depot area be evaluated as an aid to long-range planning. The Depot requested the U.S. Geological Survey to suggest study plans to accomplish an evaluation of the ground-water resources.
    [Show full text]
  • UTEP) Geological Sciences
    S. Pon1, D. De los Santos1, G. Alvarez-Rodriguez1, F. Enriquez1 S. Terrazas1, S. Terrazas1, J. Ricketts1, J.G. Olgin1,2, 1University of Texas at El Paso – Geological Sciences (500 University, El Paso, TX 79968), 2El Paso Community College – Physics Department (9570 Gateway N. Blvd, El Paso, TX 79924) Sarah Michelle Pon Deandra De Los Santos I am a senior at The University of Texas at El Paso, studying I am a senior at the University of Texas at El Paso (UTEP) Geological Sciences. I am excited to bring ideas and concepts of majoring in Geological Sciences and will graduate May, 2018. Abstract geology and planetary sciences to students. Whether it be During my time at UTEP, I have presented on salt diapirs and students who are pressuring a career in the sciences or students their possible entrainment methods at the Geological Society of just fulfilling their requirements. My goal with EIPS is to engage America conference in San Antonio. I also assisted Kuwanna Future Progress all students and get them asking questions and have them search Dyer-Pietras, a SUNY Binghampton University PhD candidate, The number of underrepresented minorities pursuing for the answers. with her research on boundaries between Eocene rock types For this internship, I have written a lab as an introduction to deposited in the shallow and deeper lake locations of the STEM fields, specifically in the sciences, has declined in remote sensing. I give a quick overview of what remote sensing is, Piceance basin in Rifle, Colorado, this past summer. I am now Furthermore, the Spring and Fall 2018 will include recent times [1].
    [Show full text]
  • GEOLOGY and GROUND-WATER SUPPLIES of the FORT WINGATE INDIAN SCHOOL AREA, Mckinley COUNTY, NEW MEXICO
    GEOLOGICAL SURVEY CIRCULAR 360 GEOLOGY AND GROUND-WATER SUPPLIES OF THE FORT WINGATE INDIAN SCHOOL AREA, McKINLEY COUNTY, NEW MEXICO PROPERTY OT§ tJ. B. EED! DGJCAL' SURVEY PUBLIC INQUIRIES OFFICE BAN FRANC1ECQ. CALIFORNIA Prepared in cooperation with the Bureau of Indian Affairs UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director GEOLOGICAL SURVEY CIRCULAR 360 GEOLOGY AND GROUND-WATER SUPPLIES OF THE FORT WINGATE INDIAN SCHOOL AREA, McKINLEY COUNTY, NEW MEXICO By J. T. Callahan and R. L. Cushman Prepared in cooperation with the Bureau of Indian Affairs Washington, D. C-, 1905 Free on application to the Geological Survey, Washington 25, D. C. GEOLOGY AND GROUND-WATER SUPPLIES OF THE FORT WINGATE INDIAN SCHOOL AREA, McKINLEY COUNTY, NEW MEXICO By J. T. Callahan and R. L. Cushman CONTENTS Page Page Abstract.................................................... 1 Geology and ground-water resources--Continued Introduction............................................... 2 Geologic structures--Continued Location, topography, and drainage............... 2 Faults..,................................................. 5 Geology and ground-water resources.............. 2 Ground water................................................ 5 Geologic formations and their water-bearing San Andres formation.................................. 5 properties........................................ 2 Recharge conditions................................. 5 Permian system................................... 4 Discharge
    [Show full text]
  • Permophiles Issue
    Contents Notes from the SPS Secretary ...........................................................................................................................1 Shen Shuzhong Notes from the SPS Chair ..................................................................................................................................2 Charles M. Henderson Meeting Report: Report on the Continental Siena Meeting, Italy, September 2006.....................................3 G. Cassinis, A. Lazzarotto, P. Pittau Working Group Report: Short report on 2005-2006 activities of the non-marine – marine correlation work- ing group of SPS ..................................................................................................................................................5 J.W. Schneider Report of SPS Working Group on “Using Permian transitional biotas as gateways for global correlation”7 Guang R. Shi International Permian Time Scale ...................................................................................................................10 Voting Members of the SPS ............................................................................................................................. 11 Submission guideline for Issue 49 ....................................................................................................................12 Reports: Ostracods (Crustacea) from the Permian-Triassic boundary interval of South China (Huaying Mountains, eastern Sichuan Province): paleo-oxygenation significance .......................................................12
    [Show full text]
  • The Largest Tropical Peat Mires in Earth History
    Geological Society of America Special Paper 370 2003 Desmoinesian coal beds of the Eastern Interior and surrounding basins: The largest tropical peat mires in Earth history Stephen F. Greb William M. Andrews Cortland F. Eble Kentucky Geological Survey, University of Kentucky, Lexington, Kentucky 40506, USA William DiMichele Smithsonian Institution, National Museum of Natural History, Washington, D.C., USA C. Blaine Cecil U.S. Geological Survey, Reston, Virginia, USA James C. Hower Center for Applied Energy Research, University of Kentucky, Lexington, Kentucky, USA ABSTRACT The Colchester, Springfield, and Herrin Coals of the Eastern Interior Basin are some of the most extensive coal beds in North America, if not the world. The Colchester covers an area of more than 100,000 km^, the Springfield covers 73,500-81,000 km^, and the Herrin spans 73,900 km^. Each has correlatives in the Western Interior Basin, such that their entire regional extent varies from 116,000 km^to 200,000 km^. Correlatives in the Appalachian Basin may indicate an even more widespread area of Desmoinesian peatland development, although possibly sUghtly younger in age. The Colchester Coal is thin, but the Springfield and Herrin Coals reach thicknesses in excess of 3 m. High ash yields, dominance of vitrinite macerals, and abundant lycopsids suggest that these Desmoinesian coals were deposited in topogenous (groundwater fed) to solige- nous (mixed-water source) mires. The only modern mire complexes that are as wide- spread are northern-latitude raised-bog mires, but Desmoinesian
    [Show full text]
  • Stratigraphic Correlation Chart for Western Colorado and Northwestern New Mexico
    New Mexico Geological Society Guidebook, 32nd Field Conference, Western Slope Colorado, 1981 75 STRATIGRAPHIC CORRELATION CHART FOR WESTERN COLORADO AND NORTHWESTERN NEW MEXICO M. E. MacLACHLAN U.S. Geological Survey Denver, Colorado 80225 INTRODUCTION De Chelly Sandstone (or De Chelly Sandstone Member of the The stratigraphic nomenclature applied in various parts of west- Cutler Formation) of the west side of the basin is thought to ern Colorado, northwestern New Mexico, and a small part of east- correlate with the Glorieta Sandstone of the south side of the central Utah is summarized in the accompanying chart (fig. 1). The basin. locations of the areas, indicated by letters, are shown on the index map (fig. 2). Sources of information used in compiling the chart are Cols. B.-C. shown by numbers in brackets beneath the headings for the col- Age determinations on the Hinsdale Formation in parts of the umns. The numbers are keyed to references in an accompanying volcanic field range from 4.7 to 23.4 m.y. on basalts and 4.8 to list. Ages where known are shown by numbers in parentheses in 22.4 m.y. on rhyolites (Lipman, 1975, p. 6, p. 90-100). millions of years after the rock name or in parentheses on the line The early intermediate-composition volcanics and related rocks separating two chronostratigraphic units. include several named units of limited areal extent, but of simi- No Quaternary rocks nor small igneous bodies, such as dikes, lar age and petrology—the West Elk Breccia at Powderhorn; the have been included on this chart.
    [Show full text]
  • Permophiles Issue
    Table of Contents Notes from the SPS Secretary 1 Lucia Angiolini Notes from the SPS Chair 2 Shuzhong Shen Officers and Voting Members since August, 2012 2 Report on the First International Congress on Continental Ichnology [ICCI-2015], El Jadida, Morocco, 21-25 April, 2015 4 Hafid Saber Report on the 7th International Brachiopod Congress, May 22-25, 2015 Nanjing, China 8 Lucia Angiolini Progress report on correlation of nonmarine and marine Lower Permian strata, New Mexico, USA 10 Spencer G. Lucas, Karl Krainer, Daniel Vachard, Sebastian Voigt, William A. DiMichele, David S. Berman, Amy C. Henrici, Joerg W. Schneider, James E. Barrick Range of morphology in monolete spores from the uppermost Permian Umm Irna Formation of Jordan 17 Michael H. Stephenson Palynostratigraphy of the Permian Faraghan Formation in the Zagros Basin, Southern Iran: preliminary studies 20 Amalia Spina, Mohammad R. Aria-Nasab , Simonetta Cirilli, Michael H. Stephenson Towards a redefinition of the lower boundary of the Protochirotherium biochron 22 Fabio Massimo Petti, Massimo Bernardi, Hendrik Klein Preliminary report of new conodont records from the Permian-Triassic boundary section at Guryul ravine, Kashmir, India 24 Michael E. Brookfield, Yadong Sun The paradox of the end Permian global oceanic anoxia 26 Claudio Garbelli, Lucia Angiolini, Uwe Brand, Shuzhong Shen, Flavio Jadoul, Karem Azmy, Renato Posenato, Changqun Cao Late Carboniferous-Permian-Early Triassic Nonmarine-Marine Correlation: Call for global cooperation 28 Joerg W. Schneider, Spencer G. Lucas Example for the description of basins in the CPT Nonmarine-Marine Correlation Chart Thuringian Forest Basin, East Germany 28 Joerg W. Schneider, Ralf Werneburg, Ronny Rößler, Sebastian Voigt, Frank Scholze ANNOUNCEMENTS 36 SUBMISSION GUIDELINES FOR ISSUE 62 39 Photo 1:The Changhsingian Gyaniyma Formation (Unit 8, bedded and Unit 9, massive, light) at the Gyaniyma section, SW Tibet.
    [Show full text]