DOCSLIB.ORG

U-Pb Detrital Geochronology and Provenance Comparisons from The

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
U-Pb Detrital Geochronology and Provenance Comparisons from The New Mexico Geological Society Downloaded from: https://nmgs.nmt.edu/publications/guidebooks/70 U-Pb Detrital Geochronology and Provenance Comparisons from the Nonmarine Strata of the Dakota Group, Lytle Sandstone, and Morrison Formation in Northeastern New Mexico Samatha R. Bartnik, Brian A. Hampton, and Greg H. Mack, 2019, pp. 55-65 in: Geology of the Raton-Clayton Area, Ramos, Frank; Zimmerer, Matthew J.; Zeigler, Kate; Ulmer-Scholle, Dana, New Mexico Geological Society 70th Annual Fall Field Conference Guidebook, 168 p. This is one of many related papers that were included in the 2019 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. No material from the NMGS website, or printed and electronic publications, may be reprinted or redistributed without NMGS permission. Contact us for permission to reprint portions of any of our publications. One printed copy of any materials from the NMGS website or our print and electronic publications may be made for individual use without our permission. Teachers and students may make unlimited copies for educational use. Any other use of these materials requires explicit permission. This page is intentionally left blank to maintain order of facing pages. New Mexico Geological Society Guidebook, 70th Field Conference, Geology of the Raton-Clayton Area, 2019, p. 55-65. 55 U-PB DETRITAL GEOCHRONOLOGY AND PROVENANCE COMPARISONS FROM NONMARINE STRATA OF THE DAKOTA GROUP, LYTLE SANDSTONE, AND MORRISON FORMATION IN NORTHEASTERN NEW MEXICO SAMANTHA R. BARTNIK, BRIAN A. HAMPTON, AND GREG H. MACK Department of Geological Sciences, New Mexico State University, Las Cruces, NM 88003, [email protected] ABSTRACT — U-Pb detrital zircon ages from sedimentary rocks of the Early–Late Cretaceous (Albian–Cenomanian) Dakota Group, Late Jurassic–Early Cretaceous(?) Lytle Sandstone, and Late Jurassic (Tithonian) Morrison Formation in northeastern New Mexico provide new geochronologic and provenance constraints on the age range and sources of detritus delivered to the Cordilleran foreland basin during Jurassic–Cretaceous time. Presented here are four U-Pb age spectra (n=978 analyses) from detrital zircons extracted from nonmarine stratigraphic horizons from these units where they crop out in the western Dry Cimarron Valley and near the Creston anticline just west of Las Vegas, New Mexico. All four stratigraphic units share strong similarities in the distribution of Paleo–Mesoproterozoic zircon ages with the majority falling between 1800–1600 (Yavapai-Mazatzal provinces), 1450–1350 (A-type granitoids), and 1300–1000 Ma (Grenville province). Neoproteozoic–Jurassic peak ages are also similar across all units with primary peaks occurring between 625–595, 430–415, 190–150 Ma. Neoproteozoic and early Paleozoic ages overlap ages of recycled Mesozoic eolionites of the Colorado plateau, whereas Jurassic ages overlap ages of magmatic sources of the Cordilleran arc. Although the Dakota Group contains elevated occurrences of Ear- ly–Late Cretaceous-age zircons with peak ages between 105–95 and 125–120 Ma, there are no occurrences of zircons younger than Late Jurassic in either the Morrison Formation or Lytle Sandstone. The nine youngest ages from the Morrison Formation fall between Early–Late Jurassic (between ~190–150 Ma), whereas the nine youngest ages from the Lytle are between Middle–Late Jurassic (~172–150 Ma). The nine youngest ages from overlying strata of the Mesa Rica Sandstone and Pajarito Formation are all Late Cretaceous (Cenomanian–earliest Turonian) and occur between ~100–92 Ma. The youngest detrital zircon ages from the Morrison Formation and Lytle Sandstone support a Late Jurassic (Tithonian) age for these units, whereas the youngest ages from both members of the Dakota Group indicate an age of earliest Late Cretaceous (Cenomanian). However, it is certainly possible that the youngest Cretaceous zircons in the Dakota Group originated from reworked, air-fall tuffs (rather than fluvial, water-laid deposits), thus the absence of these Cretaceous grains in the Lytle Sandstone could have resulted from a temporary hiatus in deposition of air-fall material to the Lytle Sandstone during the Early Cretaceous. INTRODUCTION Cordilleran arc. However, there has been very little focus on determining the provenance and further constraining the age of The Mesozoic Cordilleran foreland basin is located in the these strata (e.g., Lytle Sandstone) in northeastern New Mexico. western part of North America and is one of the best exposed The focus of this study is on provenance and formation-age and more widely studied foreland systems in the Western Hemi- relationships between nonmarine synorogenic strata of the Ear- sphere (e.g., Heller et al., 1986; Coney and Evenchick, 1994; ly–Late Cretaceous (Albian–Cenomanian) Dakota Group, the DeCelles and Currie, 1996; DeCelles, 2004; Dickinson, 2004; Late Jurassic–Early Cretaceous(?) Lytle Sandstone, and latest Fuentes et al., 2011; Lawton and Bradford, 2011; Laskowski et Jurassic (Tithonian) Morrison Formation in northeastern New al., 2013; Lawton et al., 2014; Leary et al., 2015; Yonkee and Mexico (Figs. 1, 2). Presented here are four U-Pb detrital zir- Weil, 2015). The stratigraphic response to normal subduction con age spectra from nonmarine portions of the Dakota Group, of the Farallon plate beneath North America during the Juras- Lytle Sandstone, and uppermost Morrison Formation that crop sic–Early Cretaceous and the subsequent Late Cretaceous tran- out in the western Great Plains near the western Dry Cimarron sition from flexural to dynamic subsidence across the foreland Valley and Laramide-age Crestone anticline just west of Las has been well studied (e.g., Cross and Pilger, 1978; Mitrovica Vegas, New Mexico (Fig. 1). New ages from these strata help et al., 1989; Pang and Nummedal, 1995; DeCelles and Currie, constrain upsection provenance trends in the distal parts of the 1996; Currie, 1998; DeCelles, 2004; Painter and Carrapa, 2013; Cordilleran foreland and allow for determining some of the Leary et al., 2015) and is preserved in Late Jurassic–Late Creta- youngest detritus sourced to the basin during latest Jurassic– ceous foreland basin strata throughout parts of the western U.S. Cretaceous time. Results from this study are presented and Late Jurassic–Cretaceous strata crop out throughout much of discussed in the context of provenance and age relationships central and northern New Mexico and are thought to record the across nonmarine units in the study area with the specific goal initial phase of sedimentation in the distal foreland associated of determining the youngest zircon ages in the Lytle Sandstone with normal subduction and accompanying deformation within and comparing them to the underlying Morrison Formation the Sevier fold-thrust belt and magmatism and volcanism in the and overlying Dakota Group. 56 BARTNIK, HAMPTON, AND MACK Bartnik et al._FIGURE_01 TKr TiTi Ql 104°W TKr N StudyTKpc 1 Area Ql TKpr Raton Ql KpnKvt Raton Ku Ql Qa N E W TKpcTKpc M E X I C O TKpc Tnb Ti Tim Tim Tnr 0 150 Km Ku 0 100 Km Ql Ql TiTi Tsf Kc Ti Kpn Ti TKpc Ql Ti Qv Ti Ql Ql Ti Ti Ti Ti Ti Ti J Qp Ti Ti Qa Qb Ti Ti Ti J Qa Ti Ti ^cJ ^c ^c J Ti Kvt Ti Qa Qp ^c Ti Qa J Qe Kc Ti Tus Ti Knf Knf Kc Kc J Qa Knf Tus Kpn Kc Kc QeKnf Tus G E O L O G I C M A P L E G E N D Kc ^cJ Quaternary (Pleistocene-Holocene)Qa alluvium Qa (undivided) M Quaternary (Pleistocene-Holocene) volcanic rocks (undivided) M Tmb Paleogene-Neogene (Oligocene-Pliocene) sedimentary rocks ^cu * FR 2151 (undivided); includes the Mio.-Pliocene Ogallala Formation ^cu J To 36°N Paleogene-Neogene plutonic and volcanic rocks *M Kc ^cu J (undivided) M ^c J ^c Late Cretaceous-Paleogene (Turonian-Eocene) sedimentary rocks (undivided)J ^c Early-Late Cretaceous sedimentary rocks of the Dakota Jm Group, Glencairn Formation, and Lytle Sandstone Jm Middle-Late ^cuJurassic sedimentary rocks; includes Late KdgJurassic rocks of the Morrison Formation Cambrian-Early Jurassic sedimentary rocks (undivided); To includes the Triassic Chinle Formation J NM 419 Paleo-MesoproterozoicKdg plutonic and metasedimentary rocks ^cu (undivided) Las Las VegasVegas Cenozoic faults F I E L D L O C A L I T I E S ^c2 Western Dry Cimarron Major interstates and 1 ^cu Valley - WDC * highways Jm Creston Anticline (Las Jsr Major towns 2 105°W J Vegas) - CA FIGURE 1. Generalized geologic map showing parts of northeastern New Mexico with emphasis on Late Jurassic–Late Cretaceous sedimentary rocks of the Dakota Group, Lytle Sandstone, and Morrison Formation. Geologic and geographic data from New Mexico Bureau of Geology MR, 2003 data base NMBGMR, 2003. Bartnik et al._FIGURE_02 U-PB DETRITAL GEOCHRONOLOGY AND PROVENANCE COMPARISONS FROM NONMARINE STRATA 57 N (1) WDC A Study Raton B NE Area (1) Western Dry Cimarron Valley - WDC Graneros Shale N E W Romeroville M E X I C O .
Load more

Recommended publications
  • Sediment Transport in the San Francisco Bay Coastal System: an Overview
    Marine Geology 345 (2013) 3–17 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Sediment transport in the San Francisco Bay Coastal System: An overview Patrick L. Barnard a,⁎, David H. Schoellhamer b,c, Bruce E. Jaffe a, Lester J. McKee d a U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA, USA b U.S. Geological Survey, California Water Science Center, Sacramento, CA, USA c University of California, Davis, USA d San Francisco Estuary Institute, Richmond, CA, USA article info abstract Article history: The papers in this special issue feature state-of-the-art approaches to understanding the physical processes Received 29 March 2012 related to sediment transport and geomorphology of complex coastal–estuarine systems. Here we focus on Received in revised form 9 April 2013 the San Francisco Bay Coastal System, extending from the lower San Joaquin–Sacramento Delta, through the Accepted 13 April 2013 Bay, and along the adjacent outer Pacific Coast. San Francisco Bay is an urbanized estuary that is impacted by Available online 20 April 2013 numerous anthropogenic activities common to many large estuaries, including a mining legacy, channel dredging, aggregate mining, reservoirs, freshwater diversion, watershed modifications, urban run-off, ship traffic, exotic Keywords: sediment transport species introductions, land reclamation, and wetland restoration. The Golden Gate strait is the sole inlet 9 3 estuaries connecting the Bay to the Pacific Ocean, and serves as the conduit for a tidal flow of ~8 × 10 m /day, in addition circulation to the transport of mud, sand, biogenic material, nutrients, and pollutants.
    [Show full text]
  • 112 Appendix B Hydrogeologic and Soils Factors
    APPENDIX B HYDROGEOLOGIC AND SOILS FACTORS INFLUENCING LEAKAGE POTENTIAL FROM THE CONCHAS-HUDSON CANAL SYSTEM, ARCH HURLEY CONSERVANCY DISTRICT, QUAY AND SAN MIGUEL COUNTIES, NEW MEXICO by John W. Hawley, Senior Hydrogeologist New Mexico Water Resources Research Institute and John F. Kennedy, GIS Specialist/Hydrogeologist New Mexico Water Resources Research Institute October 2005 INTRODUCTION The following discussion of geology and soils in the Arch Hurley Conservancy District (District) study area introduces the major landscape features (landforms) and surficial geologic units of the Conchas-Hudson Canal system between Conchas Reservoir in San Miguel County and the eastern part of the Tucumcari (irrigation) Project in Quay County. Emphasis is on hydrogeologic and soils factors that influence leakage from not only the canal corridor but also the complex network of laterals, ditches and field- drainage features that characterize irrigated parts of the District. Of particular importance is the historic role played by Project operations (since 1946) in recharge of the shallow- alluvial and bedrock (Entrada Sandstone) aquifer systems of the Tucumcari Metropolitan area. The latter topic was first addressed in detail by Trauger and Bushman (1964) and is only briefly covered here. 112 The geologic setting of the entire study area is the subject of a recent comprehensive review paper that was written specifically for a general audience by Adrian Hunt (Director, New Mexico Museum of Natural History and Science; 1998). Hydrogeologic characteristics of major stratigraphic units exposed or shallowly buried along the canal corridor are summarized in Table B1, which also includes a list of supporting references. Distribution patterns and leakage potential of surficial-geologic units and soils are summarized in Tables B2-B5 in Attachment B1 to this Appendix.
    [Show full text]
  • Sedimentary Provenance Studies
    Downloaded from http://sp.lyellcollection.org/ by guest on October 1, 2021 Sedimentary provenance studies P. D. W. HAUGHTON 1, S. P. TODD 2 & A. C. MORTON 3 1 Department of Geology and Applied Geology, University of Glasgow, Glasgow G12 8QQ, UK 2 BP Exploration, Britannic House, Moor Lane, London, EC2Y 9BU, UK SBritish Geological Survey, Keyworth, Nottingham NG12 5GG, UK The study of sedimentary provenance interfaces review by looking briefly at the framework several of the mainstream geological disciplines within which provenance studies are undertaken. (mineralogy, geochemistry, geochronology, sedi- mentology, igneous and metamorphic petro- logy). Its remit includes the location and nature A requisite framework for provenance of sediment source areas, the pathways by which studies sediment is transferred from source to basin of deposition, and the factors that influence the The validity and scope of any provenance study, composition of sedimentary rocks (e.g. relief, and the strategy used, are determined by a climate, tectonic setting). Materials subject to number of attributes of the targeted sediment/ study are as diverse as recent muds in the Missis- sedimentary rock (e.g. grain-size, degree of sipi River basin (Potter et al. 1975), Archaean weathering, availability of dispersal data, extent shales (McLennan et al. 1983), and soils on the of diagenetic overprint etc.). For most appli- Moon (Basu et al. 1988). cations, the location of the source is critical, and A range of increasingly sophisticated tech- ancillary data constraining this are necessary. niques is now available to workers concerned These data should limit both the direction in with sediment provenance.
    [Show full text]
  • A Combined Petrographical-Geochemical Provenance Study of the Newland Formation, Mid-Proterozoic of Montana
    223 A combined petrographical-geochemical provenance study of the Newland Formation, Mid-Proterozoic of Montana JüRGEN SCHIEBER Department of Geology, The University of Texas at Arlington (UTA), Arlington, Texas 76019, U.S.A. Abstract - A provenance study was conducted on the Mid-Proterozoic Newland Formation, in which petrographical features of sandstones and geochemical characteristics of shales were integrated to arrive at an internally consistent interpretation. Sandstones of the Newland Formation are typically arkosic sands and arkoses with very well rounded quartz and feldspar grains and only minor amounts of extrabasinal rock fragments. The predominant feldspar types are K-spar and microcline, feldspar grains are smaller than quartz grains, and feldspars show little alteration due to weathering. Detrital modes of Newland sandstones (QFL diagrams) indicate that they were derived from a stable cratonic source. These petrographical features imply a source area dominated by granites and granitoid gneisses, semi-arid to arid climate, tectonic quiescence and overall peneplain conditions. Shales of the Newland Formation are dominated by illite, quartz silt, and fine crystalline dolomite. They have small La/Th rations, relatively large Hf contents, and small contents of Cr, Co, and Ni, all indicative of derivation from crust of granitic composition. Small TiO2/AI2O3 ratios also suggest source rocks of granitic composition. The average chemical index of alteration (CIA) for Newland shales is 71.8, which in light of the probable granitoid source indicates modest amounts of chemical weathering. Relatively large Si02 contents and large K20/Na20 ratios reflect derivation from stable cratonic areas and tectonic quiescence. Thus, in general, the petrography of sandstones and geochemistry of shales provides the same provenance clues for the Newland Formation.
    [Show full text]
  • Geochemical Provenance of Clastic Sedimentary Rocks in the Western Cordillera: Utah, Colorado, Wyoming, and Oregon
    Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-2009 Geochemical Provenance of Clastic Sedimentary Rocks in the Western Cordillera: Utah, Colorado, Wyoming, and Oregon John Aaron Peterson Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Geology Commons Recommended Citation Peterson, John Aaron, "Geochemical Provenance of Clastic Sedimentary Rocks in the Western Cordillera: Utah, Colorado, Wyoming, and Oregon" (2009). All Graduate Theses and Dissertations. 439. https://digitalcommons.usu.edu/etd/439 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. GEOCHEMICAL PROVENANCE OF CLASTIC SEDIMENTARY ROCKS IN THE WESTERN CORDILLERA: UTAH, COLORADO, WYOMING, AND OREGON by John Aaron Peterson A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Geology Approved: ____________________________ ____________________________ Dr. John W. Shervais Dr. W. David Liddell Major Professor Committee Member ___________________________ ____________________________ Dr. Peter T. Kolesar Dr. Byron R. Burnham Committee Member Dean of Graduate Studies UTAH STATE UNIVERSITY Logan, Utah 2009 ii Copyright John Aaron Peterson 2009 All Rights Reserved iii ABSTRACT Geochemical Provenance of Clastic Sedimentary Rocks in the Western Cordillera: Utah, Colorado, Wyoming, and Oregon By John Aaron Peterson, Master of Science Utah State University, 2009 Major Professor: Dr. John W. Shervais Department: Geology Sedimentary rocks are an important source of information about previous orogenic conditions and the composition of which may describe the evolution of provenance and tectonic setting.
    [Show full text]
  • Mineralogical Characteristics and Geological Significance of Albian (Early Cretaceous) Glauconite in Zanda, Southwestern Tibet, China
    Clay Minerals, (2012) 47, 45–58 Mineralogical characteristics and geological significance of Albian (Early Cretaceous) glauconite in Zanda, southwestern Tibet, China 1 2, 2 2 XIANG LI , YUANFENG CAI *, XIUMIAN HU , ZHICHENG HUANG AND JIANGANG WANG2 1 Wuhan Institute of Geology and Mineral Resources, China Geological Survey, Wuhan 430223, China, and 2 State Key Laboratory for Mineral Deposits Research (Nanjing University), School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China (Received 27 November 2010; revised 9 September 2011; Editor: George Christidis) ABSTRACT: Early Cretaceous glauconite from the Xiala section, southwestern Tibet, China, was investigated by petrographic microscopy and scanning electron microscopy (SEM), X-ray diffractometry (XRD), Fourier transform infrared (FTIR) spectroscopy, and electron probe microanalysis (EPMA). The investigations revealed that the glauconite in both sandstones and limestone is highly evolved. The glauconite in sandstone is autochthonous, but in limestone it may be derived from the underlying glauconitic sandstone. Based on analyses of the depositional environments and comparisons of glauconite-bearing strata in Zanda with sequences in adjacent areas, we conclude that the glauconitization at Zanda was probably associated with rising sea levels during the Late Albian, which represent the final separation of the Indian continent from the Australian-Antarctic continent. After the separation of the Indian continent from the Australian- Antarctic continent, cooling of the Indian continent resulted in subsidence and northward subduction of the Indian plate. A gradually rising sea level in Zanda, located along the northern margin of the Indian continent, was the cause of the low sedimentation rate. Continued transgression resulted in the occurrence of the highly evolved glauconite in this area.
    [Show full text]
  • Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico
    Circular 157 1977 Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico by J. E. Gage and G. B. Asquith New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY documenting New Mexico mineral resources since 1927 Circular 157 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico by J. E. Gage and G. B. Asquith SOCORRO 1977 11 Published by Authority of State of New Mexico, NMSA 1953 Sec. 63-1-4 Printed by University of New Mexico Printing Plant, June 1977 Available from New Mexico Bureau of Mines & Mineral Resources, Socorro, NM 87801 Price $2.50 Contents iv 5 Abstract The Mesa Rica Sandstone (Lower Cretaceous) in the Tucumcari Basin of east-central New Mexico represents deposits from a lobate sand-rich delta complex. Log-probability curves of the grain-size distributions when compared to the work of Visher (1969) indicate environments ranging from distributary channels to marine wave deposits. The Mesa Rica delta prograded into the marine Tucumcari Basin from the north as shown by the south-trending to southwest-trending paleocurrent directions, and the decrease in mean grain size and thickness to the southeast, south, and southwest (lobate geometry). Also, a decrease in percent cross stratification to the southeast, south, and southwest (accompanied by an increase in percent bioturbation and burrowing) indicates a transition from predominantly fluvial to predominantly marine conditions. If the Mesa Rica Sandstone is correlative with the lower fluvial interval of the Dakota Sandstone north and northwest of the Tucumcari Basin as suggested by Scott (1970), then the Dakota Sandstone represents the fluvial facies of the Mesa Rica marine delta complex.
    [Show full text]
  • This File Copyright © the Geological Association of Canada
    This File Copyright © The Geological Association of Canada PLEASE RESPECT COPYRIGHT Considerable investment goes into the production of any publication. Recovering that investment helps ensure the publishing program can continue to provide books at reasonable prices, and continue to create publishing opportunities to future authors. This digital file is provided to the Lead Author on condition: * that the digital file remains in the possession of the Author(s), and is not distributed, shared or forwarded in any manner (except for individual study) without prior written approval from GAC®; * that the file is not manipulated in any way; * that it is understood the digital file may not be an exact representation of the original hardcopy text. As such, GAC® will be held blameless for any discrepancy between digital and printed versions; and * that printouts are distributed free of charge to colleagues and students for individual study, and do not appear in coursebooks or other compilation works (digital, printed or otherwise) for which direct or indirect payment is expected without prior arrangement with Access Copyright, the Canadian Copyright agency: Access Copyright The Canadian Copyright Licensing Agency 1 Yonge Street, Suite 800 Toronto, Ontario M5E 1E5 www.accesscopyright.ca Phone: 416-868-1620 Fax: 416-868-1621 Toll-Free: 1-800-893-5777 Email: [email protected] In the paper by Oboh-Ikuenobe et al., Table 1 (p. 206) is missing part B, as follows: Anatomy of epicontinental flooding: Late Albian-Early Cenomanian of the southern
    [Show full text]
  • Scholars Bulletin Application of Heavy Mineral Data in Provenance Analysis
    Niu Dongliang.; Sch. Bull.; Vol-2, Iss-3 (Mar, 2016):162-164 Scholars Bulletin ISSN 2412-9771 (Print) (A Multidisciplinary Journal) ISSN 2412-897X (Online) An Official Publication of “Scholars Middle East Publishers”, Dubai, United Arab Emirates Website: http://scholarsbulletin.com/ Application of heavy mineral data in provenance analysis Niu Dongliang College of earth science of Northeast Petroleum University, Daqing, Heilongjiang, China *Corresponding Author: Niu Dongliang Email: [email protected] Abstract: Heavy mineral analysis plays an important role in provenance analysis that determines the location of the source region, source spreading and feeding direction. In the detailed results of previous studies and on the basis of reading a lot of literature, this paper expounds the important role of the four heavy minerals analysis methods in provenance analysis include: the traits of heavy mineral, typomorphic characteristic, stability factor, etc., then, state the advantage and disadvantage. Keywords: heavy minerals; provenance analysis; source rock; stability. INTRODUCTION Heavy mineral analysis method is one of PROVENANCE ANALYSIS WITH THE TRAITS mature provenance analysis methods. Early heavy OF HEAVY MINERAL (TYPES, CONTENTS AND mineral analysis mainly based on its physical and DISTRIBUTION) optical properties. With the application of electronic Heavy mineral probe, the characteristic that mineral geochemical Due to the different distances or different differentiation can be fully utilized. Heavy mineral handling natural and geographical conditions, even refers to the mineral which proportion is more than 2.86 from the same deposition area, different deposits may in the sedimentary rocks, its resistance to abrasion and form individually, but the heavy mineral assemblage strong stability make it capability of more retained by they contain should be the same generally (table 1), But parent rock characteristics.
    [Show full text]
  • Making Geological Sense of 'Big Data' In
    Chemical Geology 409 (2015) 20–27 Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Making geological sense of ‘Big Data’ in sedimentary provenance analysis Pieter Vermeesch a,⁎, Eduardo Garzanti b a London Geochronology Centre, University College London, United Kingdom b Laboratory for Provenance Studies, Università di Milano-Bicocca, Italy article info abstract Article history: Sedimentary provenance studies increasingly apply multiple chemical, mineralogical and isotopic proxies to Received 14 January 2015 many samples. The resulting datasets are often so large (containing thousands of numerical values) and complex Received in revised form 30 April 2015 (comprising multiple dimensions) that it is warranted to use the Internet-era term ‘Big Data’ to describe them. Accepted 5 May 2015 This paper introduces Multidimensional Scaling (MDS), Generalised Procrustes Analysis (GPA) and Individual Available online 15 May 2015 Differences Scaling (INDSCAL, a type of ‘3-way MDS’ algorithm) as simple yet powerful tools to extract geological ‘ ’ Editor: K. Mezger insights from Big Data in a provenance context. Using a dataset from the Namib Sand Sea as a test case, we show how MDS can be used to visualise the similarities and differences between 16 fluvial and aeolian sand samples for Keywords: five different provenance proxies, resulting in five different ‘configurations’.Theseconfigurations can be fed into Provenance a GPA algorithm, which translates, rotates, scales and reflects them to extract a ‘consensus view’ for all the data Statistics considered together. Alternatively, the five proxies can be jointly analysed by INDSCAL, which fits the data with Sediments not one but two sets of coordinates: the ‘group configuration’, which strongly resembles the graphical output – U Pb produced by GPA, and the ‘source weights’, which can be used to attach geological meaning to the group config- Zircon uration.
    [Show full text]
  • GEOLOGIC TIME SCALE V
    GSA GEOLOGIC TIME SCALE v. 4.0 CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST HIST. ANOM. (Ma) ANOM. CHRON. CHRO HOLOCENE 1 C1 QUATER- 0.01 30 C30 66.0 541 CALABRIAN NARY PLEISTOCENE* 1.8 31 C31 MAASTRICHTIAN 252 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 Lopin- 254 32 C32 72.1 635 2A C2A PIACENZIAN WUCHIAPINGIAN PLIOCENE 3.6 gian 33 260 260 3 ZANCLEAN CAPITANIAN NEOPRO- 5 C3 CAMPANIAN Guada- 265 750 CRYOGENIAN 5.3 80 C33 WORDIAN TEROZOIC 3A MESSINIAN LATE lupian 269 C3A 83.6 ROADIAN 272 850 7.2 SANTONIAN 4 KUNGURIAN C4 86.3 279 TONIAN CONIACIAN 280 4A Cisura- C4A TORTONIAN 90 89.8 1000 1000 PERMIAN ARTINSKIAN 10 5 TURONIAN lian C5 93.9 290 SAKMARIAN STENIAN 11.6 CENOMANIAN 296 SERRAVALLIAN 34 C34 ASSELIAN 299 5A 100 100 300 GZHELIAN 1200 C5A 13.8 LATE 304 KASIMOVIAN 307 1250 MESOPRO- 15 LANGHIAN ECTASIAN 5B C5B ALBIAN MIDDLE MOSCOVIAN 16.0 TEROZOIC 5C C5C 110 VANIAN 315 PENNSYL- 1400 EARLY 5D C5D MIOCENE 113 320 BASHKIRIAN 323 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 1500 CALYMMIAN 6 C6 APTIAN LATE 20 120 331 6A C6A 20.4 EARLY 1600 M0r 126 6B C6B AQUITANIAN M1 340 MIDDLE VISEAN MISSIS- M3 BARREMIAN SIPPIAN STATHERIAN C6C 23.0 6C 130 M5 CRETACEOUS 131 347 1750 HAUTERIVIAN 7 C7 CARBONIFEROUS EARLY TOURNAISIAN 1800 M10 134 25 7A C7A 359 8 C8 CHATTIAN VALANGINIAN M12 360 140 M14 139 FAMENNIAN OROSIRIAN 9 C9 M16 28.1 M18 BERRIASIAN 2000 PROTEROZOIC 10 C10 LATE
    [Show full text]
  • Report 2015–1087
    Chronostratigraphic Cross Section of Cretaceous Formations in Western Montana, Western Wyoming, Eastern Utah, Northeastern Arizona, and Northwestern New Mexico, U.S.A. Pamphlet to accompany Open-File Report 2015–1087 U.S. Department of the Interior U.S. Geological Survey Chronostratigraphic Cross Section of Cretaceous Formations in Western Montana, Western Wyoming, Eastern Utah, Northeastern Arizona, and Northwestern New Mexico, U.S.A. By E.A. Merewether and K.C. McKinney Pamphlet to accompany Open-File Report 2015–1087 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, Acting 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. 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: Merewether, E.A., and McKinney, K.C., 2015, Chronostratigraphic cross section of Cretaceous formations in western Montana, western Wyoming, eastern Utah, northeastern Arizona, and northwestern New Mexico, U.S.A.: U.S. Geological Survey Open-File Report 2015–1087, 10 p.
    [Show full text]