Petroleum Geology, Resources—North Caspian Basin, Kazakhstan and Russia

Total Page:16

File Type:pdf, Size:1020Kb

Petroleum Geology, Resources—North Caspian Basin, Kazakhstan and Russia Petroleum Geology and Resources of the North Caspian Basin, Kazakhstan and Russia By Gregory F. Ulmishek U.S. Geological Survey Bulletin 2201-B U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director Version 1.0, 2001 This publication is only available online at: http://geology.cr.usgs.gov/pub/bulletins/b2201-b/ Manuscript approved for publication May 24, 2001 Published in the Central Region, Denver, Colorado Graphics by Susan Walden and Gayle M. Dumonceaux Photocomposition by Gayle M. Dumonceaux Edited by L.M. Carter Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Contents Foreword ....................................................................................................................................... 1 Abstract ......................................................................................................................................... 1 Introduction .................................................................................................................................. 2 Province Overview ....................................................................................................................... 2 Province Location and Boundaries ................................................................................ 2 Tectono-Stratigraphic Development.............................................................................. 8 Present-Day Structure ...................................................................................................... 8 Total Petroleum System.................................................................................................... 8 North Caspian Paleozoic Total Petroleum System ................................................................. 9 Overview.............................................................................................................................. 9 Discovery History...............................................................................................................9 Petroleum Occurrence...................................................................................................... 9 Stratigraphy of Subsalt Upper Paleozoic Rocks........................................................... 9 North and West Basin Margin................................................................................ 10 East-Southeast Basin Margin................................................................................. 10 South Basin Margin.................................................................................................. 10 Source Rocks...................................................................................................................... 17 Reservoir Rocks .................................................................................................................19 Seal Rocks........................................................................................................................... 19 Traps .................................................................................................................................... 21 Assessment Units .............................................................................................................. 21 Assessment Unit 10160102, North and West Margin Subsalt Barrier Reefs ............................................................................................................. 21 Assessment Unit 10160101, North and West Margin Subsalt Pinnacle Reefs .......................................................................................................... 21 Assessment Unit 10160103, East and Southeast Margin Subsalt..................... 22 Assessment Unit 10160104, South Margin Subsalt ............................................. 22 Assessment Unit 10160105, Basin Center Subsalt .............................................. 23 Assessment Unit 10160106, Suprasalt................................................................... 23 References Cited ......................................................................................................................... 23 Figures 1. Map showing petroleum system and assessment units of North Caspian basin ...................................................................................................... 3 2. Structural map of North Caspian basin...................................................................... 7 3–6. Cross sections: 3. Through north basin margin ................................................................................... 11 4. Through Karachaganak carbonate buildup......................................................... 12 III 5. Through east basin margin .................................................................................... 13 6. Of Karaton-Tengiz zone ........................................................................................... 14 7. Sketch map showing areas of carbonate buildups of northern Caspian Sea .... 15 8. Cross section of Astrakhan arch................................................................................. 16 9. Events chart of North Caspian Paleozoic Total Petroleum System ...................... 18 10. Tectonic map of northern part of east basin margin and adjacent Ural foldbelt .................................................................................................................... 20 Table 1. North Caspian basin, province 1016 assessment results summary— allocated resources...................................................................................................... 4 IV Petroleum Geology and Resources of the North Caspian Basin, Kazakhstan and Russia By Gregory F. Ulmishek Foreword Region, single digit 3 Province, three digits to the right of region code 3162 Total petroleum system, two digits to the right of This report was prepared as part of the World Energy province code 316205 Project of the U.S. Geological Survey. In the project, the world Assessment unit, two digits to the right of petroleum was divided into 8 regions and 937 geologic provinces. The system code 31620504 provinces have been ranked according to the discovered oil and The codes for the regions and provinces are listed in U.S. Geo- gas volumes within each (U.S. Geological Survey World Energy logical Survey World Energy Assessment Team (2000). Assessment Team, 2000). Then, 76 “priority” provinces (exclu- Oil and gas reserves quoted in this report are derived sive of the U.S. and chosen for their high ranking) and 26 from Petroleum Exploration and Production database (Petro- “boutique” provinces (exclusive of the U.S. and chosen for their consultants, 1996) and other area reports from Petroconsult- anticipated petroleum richness or special regional economic ants, Inc., unless otherwise noted. importance) were selected for appraisal of oil and gas resources. A map, figure 1 of this report, shows boundaries of the The petroleum geology of these priority and boutique provinces total petroleum system and assessment units; it was compiled is described in this series of reports. using geographic information system (GIS) software. Political The purpose of this effort is to aid in assessing the quanti- boundaries and cartographic representations were taken, with ties of oil, gas, and natural gas liquids that have the potential to permission, from Environmental Systems Research Institute’s be added to reserves within the next 30 years. These volumes ArcWorld 1:3 million digital coverage (1992), have no political either reside in undiscovered fields whose sizes exceed the significance, and are displayed for general reference only. Oil stated minimum-field-size cutoff value for the assessment unit and gas field centerpoints, shown on this map, are reproduced, (variable, but must be at least 1 million barrels of oil equivalent) with permission, from Petroconsultants, 1996. or occur as reserve growth of fields already discovered. The petroleum system constitutes the basic geologic unit of the oil and gas assessment. The total petroleum system includes all genetically related petroleum found in shows and accumula- Abstract tions (discovered and undiscovered) that has been generated by a pod or by closely related pods of mature source rock. This The North Caspian basin is a petroleum-rich but lightly petroleum exists within a limited mappable geologic space, explored basin located in Kazakhstan and Russia. It occupies together with the essential mappable geologic elements (source, the shallow northern portion of the Caspian Sea and a large reservoir, and seal) that control the fundamental processes of plain to the north of the sea between the Volga and Ural Rivers generation, expulsion, migration, entrapment, and preservation and farther east to the Mugodzhary Highland, which is the of petroleum. southern continuation of the Ural foldbelt. The basin is An assessment unit is a mappable part of a total petroleum bounded by the Paleozoic carbonate platform of the Volga-Ural system in which discovered and undiscovered fields constitute a province to the north and west and by the Ural, South Emba, single relatively homogeneous population such that the chosen and Karpinsky Hercynian foldbelts to the east and south. The methodology of resource assessment based on estimation of the basin was originated by pre-Late
Recommended publications
  • Oil Pollution in the Black and Caspian Seas
    Article Satellite Survey of Inner Seas: Oil Pollution in the Black and Caspian Seas Marina Mityagina and Olga Lavrova * Space Research Institute of Russian Academy of Sciences, Moscow 117997, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-495-333-4256 Academic Editors: Elijah Ramsey III, Ira Leifer, Bill Lehr, Xiaofeng Li and Prasad S. Thenkabail Received: 5 June 2016; Accepted: 17 October 2016; Published: 23 October 2016 Abstract: The paper discusses our studies of oil pollution in the Black and Caspian Seas. The research was based on a multi-sensor approach on satellite survey data. A combined analysis of oil film signatures in satellite synthetic aperture radar (SAR) and optical imagery was performed. Maps of oil spills detected in satellite imagery of the whole aquatic area of the Black Sea and the Middle and the Southern Caspian Sea are created. Areas of the heaviest pollution are outlined. It is shown that the main types of sea surface oil pollution are ship discharges and natural marine hydrocarbon seepages. For each type of pollution and each sea, regions of regular pollution occurrence were determined, polluted areas were estimated, and specific manifestation features were revealed. Long-term observations demonstrate that in recent years, illegal wastewater discharges into the Black Sea have become very common, which raises serious environmental issues. Manifestations of seabed hydrocarbon seepages were also detected in the Black Sea, primarily in its eastern part. The patterns of surface oil pollution of the Caspian Sea differ considerably from those observed in the Black Sea. They are largely determined by presence of big seabed oil and gas deposits.
    [Show full text]
  • 3. Energy Reserves, Pipeline Routes and the Legal Regime in the Caspian Sea
    3. Energy reserves, pipeline routes and the legal regime in the Caspian Sea John Roberts I. The energy reserves and production potential of the Caspian The issue of Caspian energy development has been dominated by four factors. The first is uncertain oil prices. These pose a challenge both to oilfield devel- opers and to the promoters of pipelines. The boom prices of 2000, coupled with supply shortages within the Organization of the Petroleum Exporting Countries (OPEC), have made development of the resources of the Caspian area very attractive. By contrast, when oil prices hovered around the $10 per barrel level in late 1998 and early 1999, the price downturn threatened not only the viability of some of the more grandiose pipeline projects to carry Caspian oil to the outside world, but also the economics of basic oilfield exploration in the region. While there will be some fly-by-night operators who endeavour to secure swift returns in an era of high prices, the major energy developers, as well as the majority of smaller investors, will continue to predicate total production costs (including carriage to market) not exceeding $10–12 a barrel. The second is the geology and geography of the area. The importance of its geology was highlighted when two of the first four international consortia formed to look for oil in blocks off Azerbaijan where no wells had previously been drilled pulled out in the wake of poor results.1 The geography of the area involves the complex problem of export pipeline development and the chicken- and-egg question whether lack of pipelines is holding back oil and gas pro- duction or vice versa.
    [Show full text]
  • Kashagan and Tengiz
    KashaganandTengiz—CastorandPollux DanielJohnstonandDavidJohnston AdaptedfromPetroMinMagazine–15December,2001. The recently announced super giant Kashagan discovery in the Kazakhstan sector of the NorthCaspianSeaistheworld’slargestdiscovery in three decades. Kashagan, located in shallowwater,isananalogtotheonshoreTengizfieldlocatedapproximately130to150km (85miles)tothesoutheast. KashaganandTengizarethetwolargestfieldsinKazakhstan—theiroilreservesalonerival theUnitedStates22Billionbarrelsofoil,yettheyhavehardlybeguntoproduce.Tengizin 10yearsofproductionhasproducedlessthan10%ofit’srecoverablereserves.Andwhile Kashaganwasonlyjustdiscovered,thereareothersimilarstructuresintheKashaganlicense areathatareyetundrilled.Overall,thedevelopmentcostswilllikelycosttensofbillionsof dollars but revenues to the Contractor group (the oil companies) and the Kazakhstan Governmentcouldexceed onetrilliondollars . TheKashaganprospect,(Figure1)namedafterthegreatKazakhpoet,wasidentifiedbythe Soviets in the early 1970s. However, the extremely promising prospect, located in an environmentallysensitiveandhighcostenvironment,wasnotdrilledatthattime. Threewellshavebeendrilledonthestructuresincelate2000andtheprospecthaslivedupto it’spromise.Appropriately,theKashaganproduction sharingagreement (PSA) is about as 1 famousasthediscovery. Every single percentage point (1%) take (either Government or Contractor take) could representfrom$1.5to$2billioninprofitsforthefirst10billionbarrelsalone.Thisisabig one. Thediscoveryisratedat6.4to100billionbarrels. 2However,itislikelythatagoodworking
    [Show full text]
  • Central Asia's Oil and Gas Reserves
    JANUARY 23-25, 2010 THUN, SWITZERLAND EURASIA EMERGING MARKETS FORUM Central Asia’s Oil and Gas The Emerging Markets Forum was created by the Centennial Group as a not-for-prot Reserves: initiative to bring together high-level government and corporate leaders from around the To Whom Do world to engage in dialogue on the key economic, nancial and social issues facing They Matter? emerging market countries. Martha Brill Olcott The Forum is focused on some 70 emerging market economies in East and South Asia, Eurasia, Latin America and Africa that share prospects of superior economic performance, already have or seek to create a conducive business environment and are of near-term interest to private investors, both domestic and international. Our current list of EMCs is shown on the back cover. We expect this list to eveolve over time, as countries’ policies and prospects change. Further details on the Forum and its meetings may be seen on our website at http://www.emergingmarketsforum.org Emerging The Watergate Oce Building, 2600 Virginia Avenue, NW, Suite 201 Markets Forum Washington, DC 20037, USA. Tel:(1) 202 393 6663 Fax: (1) 202 393 6556 A nonprofit initiative of the Centennial Group Email: [email protected] Bringing people together to accelerate growth and well-being in emerging markets Central Asia’s Oil and Gas Reserves: To Whom Do They Matter? Martha Brill Olcott¹ Summary Iolathan-Osman gas field, a field confirmed as one of the world’s top five deposits in an independent audit It seems like anytime one opens the business section by Gaffney, Cline and Associates.
    [Show full text]
  • Special Energy Issue on Kazakhstan |April 2018
    Special Energy Issue on Kazakhstan |April 2018 CONTENTS GENERAL ........................................................................................................................... 1 OIL & GAS PRODUCTION .................................................................................................. 3 OIL & GAS EXPORT & TRANSPORTATION ......................................................................... 3 OIL & GAS INFRASTRUCTURE ........................................................................................... 5 PROCESSING & REFINERY ................................................................................................. 6 RENEWABLE ENERGY ........................................................................................................ 6 INDUSTRY EVENTS IN 2018 .............................................................................................. 7 CONTACTS ........................................................................................................................ 7 The Economic Section of the Embassy of the Kingdom of the Netherlands in Kazakhstan intends to distribute this newsletter as widely as possible among Dutch institutions, companies and persons from the Netherlands. The newsletter summarises economic news from various Kazakhstani and foreign publications and aims to provide accurate information. However, the Embassy cannot be held responsible for any mistakes or omissions in the bulletin. SPECIAL ENERGY ISSUE, April 2018 Embassy of the Kingdom of the Netherlands GENERAL
    [Show full text]
  • Naj Žirovske Reči Stopi V Čevlje Za Nova Odkritja
    Slovenščina English Naj žirovske reči Stopi v čevlje za nova odkritja The Most Žiri Things Step into our shoes and make new discoveries Naj žirovske reči The Most Žiri Things Stopi v čevlje za nova odkritja Step into our shoes and make new discoveries 1 2 3 (1) Čevelj Alpine Alpina shoe (2) Žirovska klekljana čipka Žiri bobbin lace (3) Bunker Rupnikove linije Bunker of the Rupnik Line Žirovska zgodba The Žiri Story 4 ekoč je bilo jezero. Žirovsko jezero. nce there was a lake. Lake Žiri. A huge Veliko vodno oko, ki je zrlo v nebo, Oeye of water gazing into the sky, and the Nto pa se je v svojih spremenljivih sky was able to observe its own changing razpoloženjih ogledovalo v vodnem ogledalu moods in the mirror of water nestled among sredi Žirovske kotline, sredi samih hribov in hills and forests in the midst of the Žiri basin. gozdov. Na jugu je segalo v dolino današnjih To the south, the lake reached into the valley of Brekovic, in kdo ve, ali je od tam šla pot ali present-day Brekovice, and who knows whet- vsaj steza čez prelaz do Rovt in naprej na her a trail, or at least a footpath, led from there Notranjsko, na Logaško polje, kjer je pozneje across the pass to Rovte and onward to the nastal rimski Longaticum (Logatec). Proti Notranjska region, to the Logatec Polje, where zahodu se je zajedalo v ozko dolino Osojnice, the Roman settlement of Longaticum (Logatec) od koder se je šlo v sosednjo dolino Idrijce, was later established.
    [Show full text]
  • Zhanat Kundakbayeva the HISTORY of KAZAKHSTAN FROM
    MINISTRY OF EDUCATION AND SCIENCE OF THE REPUBLIC OF KAZAKHSTAN THE AL-FARABI KAZAKH NATIONAL UNIVERSITY Zhanat Kundakbayeva THE HISTORY OF KAZAKHSTAN FROM EARLIEST PERIOD TO PRESENT TIME VOLUME I FROM EARLIEST PERIOD TO 1991 Almaty "Кazakh University" 2016 ББК 63.2 (3) К 88 Recommended for publication by Academic Council of the al-Faraby Kazakh National University’s History, Ethnology and Archeology Faculty and the decision of the Editorial-Publishing Council R e v i e w e r s: doctor of historical sciences, professor G.Habizhanova, doctor of historical sciences, B. Zhanguttin, doctor of historical sciences, professor K. Alimgazinov Kundakbayeva Zh. K 88 The History of Kazakhstan from the Earliest Period to Present time. Volume I: from Earliest period to 1991. Textbook. – Almaty: "Кazakh University", 2016. - &&&& p. ISBN 978-601-247-347-6 In first volume of the History of Kazakhstan for the students of non-historical specialties has been provided extensive materials on the history of present-day territory of Kazakhstan from the earliest period to 1991. Here found their reflection both recent developments on Kazakhstan history studies, primary sources evidences, teaching materials, control questions that help students understand better the course. Many of the disputable issues of the times are given in the historiographical view. The textbook is designed for students, teachers, undergraduates, and all, who are interested in the history of the Kazakhstan. ББК 63.3(5Каз)я72 ISBN 978-601-247-347-6 © Kundakbayeva Zhanat, 2016 © al-Faraby KazNU, 2016 INTRODUCTION Данное учебное пособие is intended to be a generally understandable and clearly organized outline of historical processes taken place on the present day territory of Kazakhstan since pre-historic time.
    [Show full text]
  • A Preliminary Survey of the Bird Life of North Dakota
    UNIVERSITY OP MICHIGAN MUSEUM OF ZOOLOGY Miscellaneous Publications No. 10 A Preliminary Survey of the Bird Life of North Dakota BY NORMAN A. WOOD ANN ARBOR, MICHIGAN PUBLISHED BY THE UNIVERSITY JULY 2, 1923 OUTLINE MAP OF NORTH DAKOTA UNIVERSI'rY OF hlICHIGAN MUSEUM OF ZOOLOGY Miscellaneous Publications No. 10 A Preliminary Survey of the Bird Life of North Dakota RY NORMAN A. WOOD ANN ARBOR, MICIIIGAN PUBLISHED BY THE UNIVERSITY JULY 2, I923 The publications of the Museum of Zoology, University of Michigart, consist of two series-the Occasional Papers and the Miscellaneous PubK- cations. Both series were founded bv Dr. Bryant Walker, Mr. Bradsl~aw I-I. Swales and Dr. W. W. Newcomb. The Occasional Papers, publication of which was begun in 1913, j-rve as a medium for the publication of brief oriqinal papers based principally upon the collections in the Museum. The papers are issued separately to libraries and specialists, and, when a sufficient nu~uberof pages have l~crn printed to make a volume, a title page, index, and table of contents are sup- plied to libraries and individuals on the mailing list for the entire series. The Miscellaneous Publications include papers on field and museum technique, monographic studies and other papers not within the scope of the Occasional Papers. The papers are published separately, and, as it is not intended that they shall be grouped into volumes, each number has a title page and, when necessary, a table of contents. ALEXANDERG. RUTHITEN, Director of the Museum of Zoology, [Jniversity ~f Michigan. A PRELIMINARY SURVEY OF THE BIRD LIFE OF NORTH DAKOTA The field studies upon which this paper is largely based were carried on during the summers of 1920 and 1921.
    [Show full text]
  • The Five Countries of Central Asia
    The Five Countries of Central Asia 55°0'E 75°0'E Kostanai Petropavlovsk 1:10 000 000 200 100 0 200 Sergeevka Kokshetau N RUSSIAN Irtyshsk Kilometers Stepniak Pavlodar FEDERATION Rudnyi 50°0'N Makinsk Aksu Zhitikara Akkol Ereimentau Dzhetyghara Atbasar Oral Esil Ekibastuz 50°0'N Ak-Say Ishi m ASTANA Irty sh Oskemen U r a Zyrianovsk l Semey Derzhavinsk Aktobe N ura Temirtau Arkalyk Chromtau Alga Karaghandy Karkaralinsk Kandygash arysu S Ayakoz Lake Zaisan Emba KAZAKHSTAN Karazhal Atyrau Emba Shakhtinsk Shalkar Balkhash Ucharal Aral S ar Lake Balkhash Ushtobe y r D ya Baikonyr Ili Tekeli PEOPLE’S REPUBLIC Kazalinsk Taldykorgan OF CHINA Fort Shevchenko Zharkent Kyzyl Orda Chui Il i Aktau Aral Sea Kapchagay Almaty Kyzylsay Zhanatas Shu Muynak Kentau Talgar Karatau Taraz Balykchy Kungrad Chimbay Turkestan Caspian Sea BISHKEK Tokmok Karakol Shymkent Talas Lake Arys Issyk-Kul Naryn 40°0'N Nukus UZBEKISTAN Lenger KYRGYZ Dashoguz Uchkuduk Naryn Urgench Tash-Kumyr REPUBLIC TASHKENT 40°0'N Chardak Jalal Abad Khiva Zarafshan Lebap Namangan Kyzyl-Kaya Akhangaran Andizhan AZERBAIJAN Turkmenbashi Nurata Gulistan Osh Khudzand Kokand Kyzyl-Kiya Ghizhduvan Djizzak Fergana Hazar Balkanabat Gazli Navoi National capital Isfara Bereket Zhuma TURKMENISTAN Bukhara Ura-Tyube Provincial/oblast capital Aktash Samarkand Kagan Ayni Kum Dag Seydi Serdar Karakul Pendzhekent Dzhirgital City Mubarek Kasan Rogun Sumb ar Shahrizabz Rivers and canals Baharly Turkmenabad Karshi TAJIKISTAN DUSHANBE Guzar Denau Airport (international) Etrek ASHGABAT Karabekevul Kulyab Murgab K Baisun Atrek ar Talimardzhan ak International boundaries um Mary Shurchi Khorog C Kerki an Tedzhen al Bairam-Ali Gaurdak Kurgan-Tyube Boundaries are not necessarily authoritative.
    [Show full text]
  • Tetrapod Localities from the Triassic of the SE of European Russia
    Earth-Science Reviews 60 (2002) 1–66 www.elsevier.com/locate/earscirev Tetrapod localities from the Triassic of the SE of European Russia Valentin P. Tverdokhlebova, Galina I. Tverdokhlebovaa, Mikhail V. Surkova,b, Michael J. Bentonb,* a Geological Institute of Saratov State University, Ulitsa Moskovskaya, 161, Saratov 410075, Russia b Department of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UK Received 5 November 2001; accepted 22 March 2002 Abstract Fossil tetrapods (amphibians and reptiles) have been discovered at 206 localities in the Lower and Middle Triassic of the southern Urals area of European Russia. The first sites were found in the 1940s, and subsequent surveys, from the 1960s to the present day, have revealed many more. Broad-scale stratigraphic schemes have been published, but full documentation of the rich tetrapod faunas has not been presented before. The area of richest deposits covers some 900,000 km2 of territory between Samara on the River Volga in the NW, and Orenburg and Sakmara in the SW. Continental sedimentary deposits, consisting of mudstones, siltstones, sandstones, and conglomerates deposited by rivers flowing off the Ural Mountain chain, span much of the Lower and Middle Triassic (Induan, Olenekian, Anisian, Ladinian). The succession is divided into seven successive svitas, or assemblages: Kopanskaya (Induan), Staritskaya, Kzylsaiskaya, Gostevskaya, and Petropavlovskaya (all Olenekian), Donguz (Anisian), and Bukobay (Ladinian). This succession, comprising up to 3.5 km of fluvial and lacustrine sediments, documents major climatic changes. At the beginning of the Early Triassic, arid-zone facies were widely developed, aeolian, piedmont and proluvium. These were replaced by fluvial facies, with some features indicating aridity.
    [Show full text]
  • Landscape and Climate Role in the Formation of Sturgeon Reproduction Biotopes in the Ural River (Zhaiyk)
    E3S Web of Conferences 265, 01011 (2021) https://doi.org/10.1051/e3sconf/202126501011 APEEM 2021 Landscape and Climate Role in the Formation of Sturgeon Reproduction Biotopes in the Ural River (Zhaiyk) Ekaterina V. Mikodina1, *, Gulmira M. Shalgimbaeva2 and Alexander A. Volkov1 1Russian Federal Research Institute of Fisheries and Oceanography, Russian Federation 2 Fisheries Research and Production Center, Republic Kazakhstan Abstract. Geoecology of the Ural River: landscape, climate, flora, and ichthyofaunal are given. Features of air and water temperature, winds, water sources, and balance are detailed. Information about Sturgeon fishes of the Acipenseridae family, the number of which is critical, is presented. The interaction of natural conditions and anthropogenic factors in the creature of spawning biotopes is described. 1 Introduction The Ural River flows through the territories of two countries – The Russian Federation and the Republic of Kazakhstan, i.e., it is a transboundary one. Since 2018, the Russian-Kazakh Commission has been engaged in conserving the Ural River basin's ecosystem. The state of the reserves of joint transboundary species of Caspian Sea aquatic biological resources (ABR) their study, conservation, and reproduction is a priority [1]. 2 Materials and methods Analytical and expeditionary methods were used. Expedition works were located on the Republic of Kazakhstan's territory, held 15–23 September 2016, on West Kazakhstan and Atyrau regions. The depth of the river bed at the spawning grounds was measured with a GARMIN GPSMAP 580/585 echo sounder, the current velocity was measured with an ISP- 1 hydrometric spinner at the crossings of the surveyed spawning grounds, and the water temperature was measured at the sections of the channel spawning grounds with a laboratory water thermometer.
    [Show full text]
  • Geochemical and Lu-Hf Isotope (LA-ICP-MS
    Arch & Anthropol Open Acc Archaeology Copyright& Anthropology: © Kuznetsov NB CRIMSON PUBLISHERS C Wings to the Research Open Access ISSN: 2577-1949 Research Article Geochemical and Lu-Hf Isotope Systematic of Detrital Zircons from the Ordovician Sandstones of the Sol-Iletsk Arch (Russia, Northern Caspian, Borehole Ordovician-2) Kuznetsov NB 1,2,3,4*, Belousova EA4, Romanyuk TV2,3,4 1Geological Institute, Russian Academy of Sciences, Russia 2Schmidt Institute of Physics of the Earth, Russian Academy of Science, Russia 3Gubkin Russian State University of Oil and Gas, National Research University, Russia 4Australian Research Council Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Australia *Corresponding author: Kuznetsov NB, Geological Institute, Russian Academy of Sciences, Gubkin Russian State University of Oil and Gas, Russia Submission: July 02, 2018; Published: September 20, 2018 Abstract The Sol-Iletsk arch is located at the south eastern edge of the East European platform (EEP), where EEP adjoins with the Southern Urals. The results of the integrated (U-Pb age, Lu-Hf isotopic system and trace-elements) study of detrital zircons (dZr) from the Ordovician sandstones (within Sol-Iletsk arch) reached by borehole Ordovician-2 are presented. The primary sources of Early Precambrian dZr were most likely the crystalline complexes of the Late Proterozoic Volgo-Sarmatian and Taratash orogens and Archean Volga-Uralia basement. However, for numerous dZr with ages younger 1.65Ga, it is not possible presently to unambiguously identify primary sources. Crystalline complexes with such ages are absolutely atypical for the south-eastern part of the EEP, but they occurred within parts EEP very remote from Sol-Iletsk arch and beyond EEP.
    [Show full text]