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B2201-F Front Petroleum Geology and Resources of the Baykit High Province, East Siberia, Russia By Gregory F. Ulmishek U.S. Geological Survey Bulletin 2201–F 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-f 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 Manuscript approved for publication May 31, 2001 Published in the Central Region, Denver, Colorado Graphics by Susan Walden Photocomposition by William Sowers Contents Foreword ............................................................................................................................................... 1 Abstract ................................................................................................................................................. 1 Introduction .......................................................................................................................................... 2 Province Overview .............................................................................................................................. 2 Province Location and Boundaries ......................................................................................... 2 Tectono-Stratigraphic Development ....................................................................................... 2 Present-Day Structure............................................................................................................... 9 Total Petroleum System ............................................................................................................. 9 Yenisey Foldbelt Riphean-Craton Margin Riphean Total Petroleum System ............................ 11 Discovery History and Petroleum Occurrence...................................................................... 11 Stratigraphic Section ................................................................................................................. 11 Petroleum Source Rocks........................................................................................................... 11 Reservoir Rocks .......................................................................................................................... 15 Traps.............................................................................................................................................. 17 Assessment Unit ........................................................................................................................ 17 References Cited ................................................................................................................................. 18 Figures 1. Map showing total petroleum system and assessment unit of Baykit High province 1207........................................................................................ 3 2. Contour map on top of crystalline basement of Baykit high................................................ 5 3. Map showing distribution of Riphean rocks of Siberian craton ......................................... 6 4. Generalized column of Upper Proterozoic–Paleozoic rocks of Yenisey Ridge foldbelt ................................................................................................................ 7 5. Map showing Vendian–lower Paleozoic structure of Baykit regional high.................................................................................................................... 8 6. Regional cross section of Baykit High province.................................................................... 10 7. Contour map of Yurubchen-Tokhom zone............................................................................... 12 8. Cross section of Yurubchen-Tokhom zone ............................................................................. 13 9. Composite columnar section of Riphean rocks of Yurubchen-Tokhom zone ................... 15 10. Columnar section of Vendian-Cambrian rocks ...................................................................... 17 Tables 1. Yenisey Foldbelt Riphean-Craton Margin Riphean TPS 120701 assessment results summary.......................................................................................................................... 4 III Petroleum Geology and Resources of the Baykit High Province, East Siberia, Russia By Gregory F. Ulmishek Foreword Total petroleum system, two digits to the right of province code 316205 This report was prepared as part of the World Energy Assessment unit, two digits to the right of petroleum Project of the U.S. Geological Survey. In the project, the world system code 31620504 was divided into 8 regions and 937 geologic provinces. The The codes for the regions and provinces are listed in U.S. provinces were ranked according to the discovered oil and gas Geological Survey World Energy Assessment Team (2000). volumes within each (U.S. Geological Survey World Energy Oil and gas reserves quoted in this report are derived from Assessment Team, 2000). Then 76 “priority” provinces (exclu­ Petroleum Exploration and Production database (Petroconsult­ sive of the U.S. and chosen for their high rank) and 26 “bou­ ants, 1996) and other area reports from Petroconsultants, Inc., tique” provinces (exclusive of the U.S. and chosen for their unless otherwise noted. anticipated petroleum richness or special regional economic A map, figure 1 of this report, shows the boundaries of the importance) were selected for appraisal of oil and gas resources. total petroleum system and assessment unit; it was compiled The petroleum geology of these priority and boutique provinces using geographic information system (GIS) software. Political is described in this series of reports. boundaries and cartographic representations were taken, with The purpose of the World Energy Project is to aid in assess­ permission, from Environmental Systems Research Institute’s ing the quantities of oil, gas, and natural gas liquids that have a ArcWorld 1:3 million digital coverage (1992). They have no potential to be added to reserves during the next 30 years. These political significance and are displayed for general reference volumes either reside in undiscovered fields whose sizes exceed only. Oil and gas field centerpoints shown on this map are repro­ the stated minimum-field-size cutoff value for the assessment duced, with permission, from Petroconsultants (1996). unit (variable, but at least 1 million barrels of oil equivalent), or they occur as reserve growth of fields already discovered. The total petroleum system constitutes the basic geologic Abstract unit of the oil and gas assessment. The total petroleum system The Baykit High province consists of two principal struc­ includes all genetically related petroleum in shows and accumu­ tural units—the Baykit regional high in the west, which occupies lations (discovered and undiscovered) that has been generated by most of the province, and the Katanga structural saddle in the east. a pod or by closely related pods of mature source rock. This The province is on the western margin of the Siberian craton east petroleum exists within a limited mappable geologic space, of theYenisey Ridge foldbelt. The province is an exploration fron­ together with the essential mappable geologic elements (source, tier and only a few prospects have been drilled. The oldest sedi­ reservoir, and seal) that control the fundamental processes of gen­ mentary rocks of the province, Riphean carbonate and clastic eration, expulsion, migration, entrapment, and preservation of strata of Late Proterozoic age (1,650–650 million years old) that petroleum. were deposited on the passive margin, cover the Archean–Lower An assessment unit is a mappable part of a total petroleum Proterozoic basement. Basal Vendian (uppermost Proterozoic, system, in which discovered and undiscovered fields constitute a 650–570 million years old) clastic rocks unconformably overlie single relatively homogeneous population, such that the chosen various units of the Riphean and locally lie directly on the base­ methodology of resource assessment based on estimation of the ment. Younger Vendian and lowermost Cambrian rocks are number and sizes of undiscovered fields is applicable. A total primarily dolomites. The Vendian/Cambrian boundary is con- petroleum system may equate to a single assessment unit. If nec­ formable, and its exact stratigraphic position has not been identi­ essary, a total petroleum system may be divided into two or more fied with certainty. The Lower Cambrian section is thick, and it assessment units, such that each assessment unit is sufficiently consists of alternating beds of dolomite and evaporites (mostly homogeneous in terms of geology, exploration considerations, salt). Middle and Upper Cambrian strata are composed of shale and risk to be assessed individually. and dolomite. Ordovician-Silurian and upper Paleozoic rocks are A numeric code identifies each region, province, total petro­ thin, and they are present only in the northern areas of the prov­ leum system, and assessment unit; these codes are uniform ince. Structural pattern of Riphean rocks differs substantially throughout the World Energy Project and each code identifies the from that of Vendian-Cambrian rocks. same item in all publications. The
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