Geologic Map of Alaska

Total Page:16

File Type:pdf, Size:1020Kb

Geologic Map of Alaska Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey Front cover. Color shaded relief map of Alaska and surroundings. Sources: 100-meter-resolution natural image of Alaska, http://nationalmap.gov/small_scale/mld/nate100.html; rivers and lakes dataset, http://www.asgdc.state.ak.us/; bathymetry and topography of Russia and Canada, https://www.ngdc.noaa.gov/mgg/global/global.html. Back cover. Previous geologic maps of Alaska: 1906—Brooks, A.H., Abbe, Cleveland, Jr., and Goode, R.U., 1906, The geography and geology of Alaska; a summary of existing knowledge, with a section on climate, and a topographic map and description thereof: U.S. Geological Survey Professional Paper 45, 327 p., 1 sheet. 1939—Smith, P.S., 1939, Areal geology of Alaska: U.S. Geological Survey Professional Paper 192, 100 p., 18 plates. 1957—Dutro, J.T., Jr., and Payne, T.G., 1957, Geologic map of Alaska: U.S. Geological Survey, scale 1:2,500,000. 1980—Beikman, H.M., 1980, Geologic map of Alaska: U.S. Geological Survey Special Map, scale 1:2,500,000, 2 sheets. Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Wilson, F.H., Hults, C.P., Mull, C.G., and Karl, S.M., comps., 2015, Geologic map of Alaska: U.S. Geological Survey Scientific Investigations Map 3340, 197 p., 2 sheets, scale 1:584,000, http://dx.doi.org/10.3133/sim3340. ISSN 2329-1311 (print) ISSN 2329-132X (online) ISBN 978-1-4113-4000-8 Contents Introduction ....................................................................................................................................................1 Acknowledgments ........................................................................................................................................3 Description of Map Units .............................................................................................................................5 Unconsolidated Deposits ....................................................................................................................5 Sedimentary Rocks ..............................................................................................................................5 Cenozoic to Mesozoic .................................................................................................................5 Quaternary and Tertiary ....................................................................................................5 Tertiary to Mesozoic ...........................................................................................................6 Cenozoic to Paleozoic ...............................................................................................................16 Tertiary to Devonian .........................................................................................................16 Tertiary to Jurassic .................................................................................................16 Lower Cretaceous to Devonian ............................................................................ 25 Jurassic to Mississippian ............................................................................................... 35 Triassic .............................................................................................................................. 42 Paleozoic to Proterozoic .......................................................................................................... 47 Permian to Devonian ....................................................................................................... 47 Carboniferous .................................................................................................................. 49 Devonian to Neoproterozoic .......................................................................................... 55 Silurian to Cambrian ....................................................................................................... 69 Ordovician to Proterozoic ............................................................................................... 71 Cambrian to Proterozoic ................................................................................................. 73 Proterozoic ..................................................................................................................................74 Volcanic Rocks .................................................................................................................................. 75 Cenozoic to Mesozoic .............................................................................................................. 75 Quaternary to Tertiary ..................................................................................................... 75 Tertiary to Cretaceous ..................................................................................................... 76 Mesozoic .................................................................................................................................... 82 Cretaceous to Jurassic ................................................................................................... 82 Jurassic to Triassic .......................................................................................................... 84 Triassic ............................................................................................................................... 85 Paleozoic .................................................................................................................................... 86 Permian.............................................................................................................................. 86 Carboniferous ................................................................................................................... 87 Devonian............................................................................................................................ 87 Silurian ............................................................................................................................... 88 Ordovician and Cambrian ............................................................................................... 88 Proterozoic ................................................................................................................................. 88 Intrusive Rocks ................................................................................................................................... 89 Cenozoic to Mesozoic .............................................................................................................. 89 Quaternary or Tertiary ..................................................................................................... 89 Tertiary to Cretaceous ..................................................................................................... 89 Mesozoic and Paleozoic .......................................................................................................... 96 Cretaceous to Paleozoic ................................................................................................ 96 Jurassic to Paleozoic .................................................................................................... 100 Triassic to Paleozoic ...................................................................................................... 104 Paleozoic to Proterozoic ........................................................................................................ 106 Metamorphic Rocks ....................................................................................................................... 109 iii Cenozoic to Mesozoic ............................................................................................................ 109 Quaternary or Tertiary ................................................................................................... 109 Tertiary to Mesozoic ...................................................................................................... 109 Mesozoic to Proterozoic .........................................................................................................110 Cretaceous to Paleozoic ................................................................................................110 Triassic to Proterozoic
Recommended publications
  • A Classification of Living and Fossil Genera of Decapod Crustaceans
    RAFFLES BULLETIN OF ZOOLOGY 2009 Supplement No. 21: 1–109 Date of Publication: 15 Sep.2009 © National University of Singapore A CLASSIFICATION OF LIVING AND FOSSIL GENERA OF DECAPOD CRUSTACEANS Sammy De Grave1, N. Dean Pentcheff 2, Shane T. Ahyong3, Tin-Yam Chan4, Keith A. Crandall5, Peter C. Dworschak6, Darryl L. Felder7, Rodney M. Feldmann8, Charles H. J. M. Fransen9, Laura Y. D. Goulding1, Rafael Lemaitre10, Martyn E. Y. Low11, Joel W. Martin2, Peter K. L. Ng11, Carrie E. Schweitzer12, S. H. Tan11, Dale Tshudy13, Regina Wetzer2 1Oxford University Museum of Natural History, Parks Road, Oxford, OX1 3PW, United Kingdom [email protected] [email protected] 2Natural History Museum of Los Angeles County, 900 Exposition Blvd., Los Angeles, CA 90007 United States of America [email protected] [email protected] [email protected] 3Marine Biodiversity and Biosecurity, NIWA, Private Bag 14901, Kilbirnie Wellington, New Zealand [email protected] 4Institute of Marine Biology, National Taiwan Ocean University, Keelung 20224, Taiwan, Republic of China [email protected] 5Department of Biology and Monte L. Bean Life Science Museum, Brigham Young University, Provo, UT 84602 United States of America [email protected] 6Dritte Zoologische Abteilung, Naturhistorisches Museum, Wien, Austria [email protected] 7Department of Biology, University of Louisiana, Lafayette, LA 70504 United States of America [email protected] 8Department of Geology, Kent State University, Kent, OH 44242 United States of America [email protected] 9Nationaal Natuurhistorisch Museum, P. O. Box 9517, 2300 RA Leiden, The Netherlands [email protected] 10Invertebrate Zoology, Smithsonian Institution, National Museum of Natural History, 10th and Constitution Avenue, Washington, DC 20560 United States of America [email protected] 11Department of Biological Sciences, National University of Singapore, Science Drive 4, Singapore 117543 [email protected] [email protected] [email protected] 12Department of Geology, Kent State University Stark Campus, 6000 Frank Ave.
    [Show full text]
  • Handbook of Texas Cretaceous Fossils
    University of Texas Bulletin No. 2838: October 8, 1928 HANDBOOK OF TEXAS CRETACEOUS FOSSILS B y W. S. ADKINS Bureau of Economic Geology J. A. Udden, Director E. H. Sellards, Associate Director PUBLISHED BY THE UNIVERSITY FOUR TIMES A MONTH, AND ENTERED AS SECOND-CLASS MATTER AT THE POSTOFFICE AT AUSTIN, TEXAS. UNDER THE ACT OF AUGUST 24. 1912 The benefits of education and of useful knowledge, generally diffused through a community, are essential to the preservation of a free govern­ m en t. Sam Houston Cultivated mind is the guardian genius of democracy. It is the only dictator that freemen acknowl­ edge and the only security that free­ men desire. Mirabeau В. Lamar CONTENTS P age Introduction __________________________________________________ 5 Summary of Formation Nomenclature_______________________ 6 Zone Markers and Correlation_______________________________ 8 Types of Texas Cretaceous Fossils___________________________ 36 Bibliography ________________________________________________ 39 L ist and Description of Species_________________________________ 46 P lants ______________________________________________________ 46 Thallophytes ______________________________________________ 46 Fungi __________________________________________________ 46 Algae __________________________________________________ 47 Pteridophytes ____________________________________________ 47 Filices __________________________________________________ 47 Spermatophytes __________________________________________ 47 Gymnospermae _________________________________________
    [Show full text]
  • Or Early Callovian) Ammonites from Alaska and Montana
    Jurassic (Bathonian or Early Callovian) Ammonites From Alaska and Montana By RALPH W. IMLAY SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 374-C Descr$tions and illustrations of ctphalopods of possible late Middle Jurasric (Bathonian) age UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page C- 1 Age of the faunas-Continued C- 1 Callovian versus Bathonian in Greenland- - - - _ - - _ - - C-2 Callovian versus Bathonian in Alaska and Montana- -- - Stratigraphic summary- __ --______ _ - - - -- - ---.- -- -.- - - C-2 Paleogeographic considerations- - -_-- -- ---- ---- Cook Inlet region, Alaska -______--------.-.--..--c-2 Summation of the evidence- - - _._ _ - _ _ - - - - - - - - - - - - Iniskin Peninsula-_-_______----.--------~.--C-2 Comparisons with other faunas---------___----------- Peninsula north of Chinitna Bay----- __._ _ _._ - C-3 \Vestern interior of Canada- - - -- -- -____------- --- Talkeetna Mountains ----___-_ - - -- ---- - - -- - -- C-3 Arctic region-_-_---___-_----------------------- Western Montana- - -----__-----------------.---C-5 other regions--__-__-____----------------------- Rocky Mountain front north of the Sun River- (2-5 Geographic distribution ___-___ --- - ---------- ------ -- - Drummond area--- ---_____ _--- -- -.-- ---- -- - C-10 Summary of results- --_-____-_----_---_-_----------- Age ofthe faunas-----------_----------------------- GI0 Systematic descriptions--_ _ _ - _ - - - - - - - - - - - - - - - - - - - - - - - Evidence from Alaska---____________--------------C-10 Literature cited _-_-_---______----------------------- Evidence from Montana --_-_____ --- - - -- .--- --- - - C-12 Index---__--___-_-_------------------------------- ILLUSTRATIONS [Plates 1-3 follow index] PLATE 1. Holcophylloceras, Oecotraustes (Paroecotraustes) ?, and Arctocephalites (Cranocephalites). 2.
    [Show full text]
  • 1 Paleobotanical Proxies for Early Eocene Climates and Ecosystems in Northern North 2 America from Mid to High Latitudes 3 4 Christopher K
    https://doi.org/10.5194/cp-2020-32 Preprint. Discussion started: 24 March 2020 c Author(s) 2020. CC BY 4.0 License. 1 Paleobotanical proxies for early Eocene climates and ecosystems in northern North 2 America from mid to high latitudes 3 4 Christopher K. West1, David R. Greenwood2, Tammo Reichgelt3, Alexander J. Lowe4, Janelle M. 5 Vachon2, and James F. Basinger1. 6 1 Dept. of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, 7 Saskatchewan, S7N 5E2, Canada. 8 2 Dept. of Biology, Brandon University, 270-18th Street, Brandon, Manitoba R7A 6A9, Canada. 9 3 Department of Geosciences, University of Connecticut, Beach Hall, 354 Mansfield Rd #207, 10 Storrs, CT 06269, U.S.A. 11 4 Dept. of Biology, University of Washington, Seattle, WA 98195-1800, U.S.A. 12 13 Correspondence to: C.K West ([email protected]) 14 15 Abstract. Early Eocene climates were globally warm, with ice-free conditions at both poles. Early 16 Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate biota, 17 but also with abundant thermophilic elements such as crocodilians, and mesothermic taxodioid 18 conifers and angiosperms. The globally warm early Eocene was punctuated by geologically brief 19 hyperthermals such as the Paleocene-Eocene Thermal Maximum (PETM), culminating in the 20 Early Eocene Climatic Optimum (EECO), during which the range of thermophilic plants such as 21 palms extended into the Arctic. Climate models have struggled to reproduce early Eocene Arctic 22 warm winters and high precipitation, with models invoking a variety of mechanisms, from 23 atmospheric CO2 levels that are unsupported by proxy evidence, to the role of an enhanced 24 hydrological cycle to reproduce winters that experienced no direct solar energy input yet remained 25 wet and above freezing.
    [Show full text]
  • The Middle Jurassic of Western and Northern Europe: Its Subdivisions, Geochronology and Correlations
    The Middle Jurassic of western and northern Europe: its subdivisions, geochronology and correlations John H. Callomon The palaeogeographic settings of Denmark and East Greenland during the Middle Jurassic are outlined. They lay in the widespread epicontinental seas that covered much of Europe in the post-Triassic transgression. It was a period of continuing eustatic sea-level rise, with only distant connections to world oceans: to the Pacific, via the narrow Viking Straits between Greenland and Norway and hence the arctic Boreal Sea to the north; and to the subtropical Tethys, via some 1200 km of shelf-seas to the south. The sedimentary history of the region was strongly influenced by two factors: tectonism and climate. Two modes of tectonic movement governed basinal evolution: crustal extension lead- ing to subsidence through rifting, such as in the Viking and Central Grabens of the North Sea; and subcrustal thermal upwelling, leading to domal uplift and the partition of marine basins through emergent physical barriers, as exemplified by the Central North Sea Dome with its associated volcanics. The climatic gradient across the 30º of temperate latitude spanned by the European seas governed biotic diversity and biogeography, finding expression in rock-forming biogenic carbonates that dominate sediments in the south and give way to largely siliciclastic sediments in the north. Geochronology of unrivalled finesse is provided by standard chronostratigraphy based on the biostratigraphy of ammonites. The Middle Jurassic saw the onset of considerable bioprovincial endemisms in these guide-fossils, making it necessary to construct parallel standard zonations for Boreal, Subboreal or NW European and Submediterranean Provinces, of which the NW European zonation provides the primary international standard.
    [Show full text]
  • Natural Communities of Michigan: Classification and Description
    Natural Communities of Michigan: Classification and Description Prepared by: Michael A. Kost, Dennis A. Albert, Joshua G. Cohen, Bradford S. Slaughter, Rebecca K. Schillo, Christopher R. Weber, and Kim A. Chapman Michigan Natural Features Inventory P.O. Box 13036 Lansing, MI 48901-3036 For: Michigan Department of Natural Resources Wildlife Division and Forest, Mineral and Fire Management Division September 30, 2007 Report Number 2007-21 Version 1.2 Last Updated: July 9, 2010 Suggested Citation: Kost, M.A., D.A. Albert, J.G. Cohen, B.S. Slaughter, R.K. Schillo, C.R. Weber, and K.A. Chapman. 2007. Natural Communities of Michigan: Classification and Description. Michigan Natural Features Inventory, Report Number 2007-21, Lansing, MI. 314 pp. Copyright 2007 Michigan State University Board of Trustees. Michigan State University Extension programs and materials are open to all without regard to race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, marital status or family status. Cover photos: Top left, Dry Sand Prairie at Indian Lake, Newaygo County (M. Kost); top right, Limestone Bedrock Lakeshore, Summer Island, Delta County (J. Cohen); lower left, Muskeg, Luce County (J. Cohen); and lower right, Mesic Northern Forest as a matrix natural community, Porcupine Mountains Wilderness State Park, Ontonagon County (M. Kost). Acknowledgements We thank the Michigan Department of Natural Resources Wildlife Division and Forest, Mineral, and Fire Management Division for funding this effort to classify and describe the natural communities of Michigan. This work relied heavily on data collected by many present and former Michigan Natural Features Inventory (MNFI) field scientists and collaborators, including members of the Michigan Natural Areas Council.
    [Show full text]
  • Chapter 2 Darkness
    Chapter 2 Darkness f all the disconcerting statements in Veniaminov’s great work on the eastern Aleutians—and there are several—few are O more arresting than his assertion that elderly Unanga{ told of famous shamans who, long before the first Russians appeared, said white people would arrive from the sea and afterwards all Unanga{ would come to resemble them and would adopt their customs. These elders also reported that at the time of the Russian arrival the shamans began prophesizing that “in the east, over their islands,” they saw “a brilliant dawn or a great light” inhabited by “many people resembling the newcomers, while in the lower world, of the people whom they had seen there before, very few remained” and “impenetrable darkness set in.”1 This darkness surrounds the earliest history of Biorka, Kashega, and Makushin. Nick Galaktionoff joked that when people asked him where Aleuts came from, he would tell them, “Tomorrow I come from Makushin!” By “tomorrow” he meant “yesterday” or “that time before.” “I was right,” he laughed, “‘cause I was born there.”2 And yet Nick had an older origin story that began when Unanga{ lived on the mainland, a time when ice covered much of the coastline.3 Food became scarce and animals began preying on villages, taking food and attacking people. The chiefs spoke with their people and explained that they would have to go across the ice. They covered the bottoms of their open skin boats with seal skin that still had the fur on it, and this smooth surface allowed the heavily laden boats to be towed.
    [Show full text]
  • Resource Utilization in Unalaska, Aleutian Islands, Alaska
    RESOURCE UTILIZATION IN UNALASKA, ALEUTIAN ISLANDS, ALASKA Douglas W. Veltre, Ph. D. Mary J. Veltre, B.A. Technical Paper Number 58 Alaska Department of Fish and Game Division of Subsistence October 23, 1982 Contract 824790 ACKNOWLEDGMENTS This report would not have been possible to produce without the generous support the authors received from many residents of Unalaska. Numerous individuals graciously shared their time and knowledge, and the Ounalashka Corporation,. in particular, deserves special thanks for assistance with housing and transportation. Thanks go too to Linda Ellanna, Deputy Director of the Division of Subsistence, who provided continuing support throughout this project, and to those individuals who offered valuable comments on an earlier draft of this report. ii TABLE OF CONTENTS ACKNOWLEDGMENTS. ii Chapter 1 INTRODUCTION . 1 Purpose ..................... 1 Research objectives ............... 4 Research methods 6 Discussion of rese~r~h'm~tho~oio~y' ........ ...... 8 Organization of the report ........... 10 2 BACKGROUNDON ALEUT RESOURCE UTILIZATION . 11 Introduction ............... 11 Aleut distribuiiin' ............... 11 Precontact resource is: ba;tgr;ls' . 12 The early postcontact period .......... 19 Conclusions ................... 19 3 HISTORICAL BACKGROUND. 23 Introduction ........................... 23 The precontact'plrioi . 23 The Russian period ............... 25 The American period ............... 30 Unalaska community profile. ........... 37 Conclusions ................... 38 4 THE NATURAL SETTING ...............
    [Show full text]
  • Preliminary Geologic Map of the Baird Mountains and Part of the Selawik Quadrangles, Alaska By
    preliminary Geologic Map of the Baird Mountains and part of the Selawik Quadrangles, Alaska by S.M. Karl, J.A. Dumoulin, Inyo Ellersieck, A.G. Harris, and J.M. Schmidt Open-File Report 89-551 This map is preliminary and has not been reviewed for conformity 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. Table Contents ~ntroduction.......................................... 1 Stratigraphic Framework .................................1 Structural Framework ....................................4 Acknowledgments .......................................6 Unit Descriptions ......................................6 Kc ............................................. 6 KJm .............................................6 JPe .............................................7 ~zb................ '. ... ., ,....................... 8 Mzg ............................................10 MzPzi ..........................................10 MZPZ~.......................................... 11 PMC ............................................12 PD1 ............................................12 Mk0 ............................................12 M1 .............................................13 MDue ...........................................14 Mlt ............................................15 Mk .............................................15 MD1 ............................................16 MDe ............................................16 MD~...........................................
    [Show full text]
  • Fossil Mosses: What Do They Tell Us About Moss Evolution?
    Bry. Div. Evo. 043 (1): 072–097 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.7 Fossil mosses: What do they tell us about moss evolution? MicHAEL S. IGNATOV1,2 & ELENA V. MASLOVA3 1 Tsitsin Main Botanical Garden of the Russian Academy of Sciences, Moscow, Russia 2 Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia 3 Belgorod State University, Pobedy Square, 85, Belgorod, 308015 Russia �[email protected], https://orcid.org/0000-0003-1520-042X * author for correspondence: �[email protected], https://orcid.org/0000-0001-6096-6315 Abstract The moss fossil records from the Paleozoic age to the Eocene epoch are reviewed and their putative relationships to extant moss groups discussed. The incomplete preservation and lack of key characters that could define the position of an ancient moss in modern classification remain the problem. Carboniferous records are still impossible to refer to any of the modern moss taxa. Numerous Permian protosphagnalean mosses possess traits that are absent in any extant group and they are therefore treated here as an extinct lineage, whose descendants, if any remain, cannot be recognized among contemporary taxa. Non-protosphagnalean Permian mosses were also fairly diverse, representing morphotypes comparable with Dicranidae and acrocarpous Bryidae, although unequivocal representatives of these subclasses are known only since Cretaceous and Jurassic. Even though Sphagnales is one of two oldest lineages separated from the main trunk of moss phylogenetic tree, it appears in fossil state regularly only since Late Cretaceous, ca.
    [Show full text]
  • A New Classification of the Xanthoidea Sensu Lato
    Contributions to Zoology, 75 (1/2) 23-73 (2006) A new classifi cation of the Xanthoidea sensu lato (Crustacea: Decapoda: Brachyura) based on phylogenetic analysis and traditional systematics and evaluation of all fossil Xanthoidea sensu lato Hiroaki Karasawa1, Carrie E. Schweitzer2 1Mizunami Fossil Museum, Yamanouchi, Akeyo, Mizunami, Gifu 509-6132, Japan, e-mail: GHA06103@nifty. com; 2Department of Geology, Kent State University Stark Campus, 6000 Frank Ave. NW, North Canton, Ohio 44720, USA, e-mail: [email protected] Key words: Crustacea, Decapoda, Brachyura, Xanthoidea, Portunidae, systematics, phylogeny Abstract Family Pilumnidae ............................................................. 47 Family Pseudorhombilidae ............................................... 49 A phylogenetic analysis was conducted including representatives Family Trapeziidae ............................................................. 49 from all recognized extant and extinct families of the Xanthoidea Family Xanthidae ............................................................... 50 sensu lato, resulting in one new family, Hypothalassiidae. Four Superfamily Xanthoidea incertae sedis ............................... 50 xanthoid families are elevated to superfamily status, resulting in Superfamily Eriphioidea ......................................................... 51 Carpilioidea, Pilumnoidoidea, Eriphioidea, Progeryonoidea, and Family Platyxanthidae ....................................................... 52 Goneplacoidea, and numerous subfamilies are elevated
    [Show full text]
  • Thermochronology of the Talkeetna Intraoceanic Arc of Alaska: Ar/Ar, U‐Th/He, Sm‐Nd, and Lu‐Hf Dating
    TECTONICS, VOL. 30, TC1011, doi:10.1029/2010TC002798, 2011 Thermochronology of the Talkeetna intraoceanic arc of Alaska: Ar/Ar, U‐Th/He, Sm‐Nd, and Lu‐Hf dating B. R. Hacker,1 Peter B. Kelemen,2 Matthew Rioux,1,3 Michael O. McWilliams,4 Philip B. Gans,1 Peter W. Reiners,5 Paul W. Layer,6 Ulf Söderlund,7 and Jeffrey D. Vervoort8 Received 17 September 2010; revised 8 December 2010; accepted 27 December 2010; published 26 February 2011. [1] As one of two well‐exposed intraoceanic arcs, the of the Talkeetna arc was spatially variable. One‐ Talkeetna arc of Alaska affords an opportunity to under- dimensional finite difference thermal models show that stand processes deep within arcs. This study reports new this kind of spatial variability is inherent to intraoceanic Lu‐Hf and Sm‐Nd garnet ages, 40Ar/39Ar hornblende, arcs with simple construction histories. Citation: Hacker, mica and whole‐rock ages, and U‐Th/He zircon and B. R., P. B. Kelemen, M. Rioux, M. O. McWilliams, P. B. Gans, apatite ages from the Chugach Mountains, Talkeetna P. W. Reiners, P. W. Layer, U. Söderlund, and J. D. Vervoort Mountains, and Alaska Peninsula, which, in conjunc- (2011), Thermochronology of the Talkeetna intraoceanic arc of tion with existing geochronology, constrain the thermal Alaska: Ar/Ar, U‐Th/He, Sm‐Nd, and Lu‐Hf dating, Tectonics, history of the arc. Zircon U‐Pb ages establish the 30, TC1011, doi:10.1029/2010TC002798. main period of arc magmatism as 202–181 Ma in the Chugach Mountains and 183–153 Ma in the 1.
    [Show full text]