Depositional ages and characteristics of Middle–Upper Jurassic and Lower Cretaceous lacustrine deposits in southeastern Mongolia |
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| Authors: | Hitoshi Hasegawa Hisao Ando Noriko Hasebe Niiden Ichinnorov Tohru Ohta Takashi Hasegawa Masanobu Yamamoto Gang Li Bat‐Orshikh Erdenetsogt Ulrich Heimhofer Takayuki Murata Hironori Shinya G Enerel G Oyunjargal O Munkhtsetseg Noriyuki Suzuki Tomohisa Irino Koshi Yamamoto |
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| Affiliation: | 1. Department of Global Environment and Disaster Prevention, Faculty of Science and Technology, Kochi University, Kochi 780‐8520, Japan;2. University Museum, Nagoya University, Furo‐cho, Chikusa‐ku, Nagoya 464‐8601, Japan;3. Department of Earth Sciences, Faculty of Science, Ibaraki University, Bunkyo, Mito 310‐8512, Japan;4. Institute of Nature and Environmental Technology, Kanazawa University, Kakuma, Kanazawa 920‐1192, Japan;5. Institute of Paleontology and Geology, Mongolian Academy of Sciences, P.O.B. 260, Ulaanbaatar 210351, Mongolia;6. Department of Earth Sciences, Faculty of Education and Integrated Arts and Sciences, Waseda University, Nishiwaseda, Shinjuku, Tokyo 169‐8050, Japan;7. Department of Earth Sciences, Faculty of Science, Kanazawa University, Kakuma, Kanazawa 920‐1192, Japan;8. Faculty of Environmental Earth Science, Hokkaido University, Kita 8, Nishi 5, Kita‐ku, Sapporo 060‐0810, Japan;9. Nanjing Institute of Geology and Palaeontology, Chinese Academy of Science, 39 East Beijing Road, Nanjing 210008, China;10. Department of Geology and Geophysics, National University of Mongolia, KH Surguuliin Gudamj‐1, Ulaanbaatar 14200, Mongolia;11. Institute for Geology, Leibniz University Hannover, Welfengarten 1, Hannover D‐30167, Germany;12. School of Geology and Mining, Mongolian University of Science and Technology, Baga Toiruu34, Sukhbaatar, Ulaanbaatar 210646, Mongolia;13. Department of Natural History Science, Hokkaido University, Kita 8, Nishi 5, Kita‐ku, Sapporo 060‐0810, Japan;14. Graduate School of Environmental Studies, Nagoya University, Furo‐cho, Chikusa‐ku, Nagoya 464‐8601, Japan |
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| Abstract: | Lower Cretaceous lacustrine oil shales are widely distributed in southeastern Mongolia. Due to the high organic carbon content of oil shale, many geochemical studies and petroleum exploration have been conducted. Although most of the oil shales are considered to be Early Cretaceous in age, a recent study reveals that some were deposited in the Middle Jurassic. The present study aims at establishing depositional ages and characteristics of the Jurassic and Cretaceous lacustrine deposits in Mongolia. The Lower Cretaceous Shinekhudag Formation is about 250 m thick and composed of alternating beds of shale and dolomite. The Middle Jurassic Eedemt Formation is about 150 m thick and composed of alternating beds of shale, dolomitic marl, and siltstone. The alternations of shale and dolomite in both formations were formed by lake level changes, reflecting precipitation changes. Shales were deposited in the center of a deep lake during highstand, while dolomites were formed by primary precipitation during lowstand. Based on the radiometric age dating, the Shinekhudag Formation was deposited between 123.8 ±2.0 Ma and 118.5 ±0.9 Ma of the early Aptian. The Eedemt Formation was deposited at around 165–158 Ma of Callovian–Oxfordian. The calculated sedimentation rate of the Shinekhudag Formation is between 4.7 ±2.6 cm/ky and 10.0 ±7.6 cm/ky. Shales in the Shinekhudag Formation show micrometer‐scale lamination, consisting of algal organic matter and detrital clay mineral couplets. Given the average thickness of micro‐laminae and calculated sedimentation rate, the micro‐lamination is most likely of varve origin. Both Middle–Upper Jurassic and Lower Cretaceous lacustrine oil shales were deposited in intracontinental basins in the paleo‐Asian continent. Tectonic processes and basin evolution basically controlled the deposition of these oil shales. In addition, enhanced precipitation under humid climate during the early Aptian and the Callovian–Oxfordian was another key factor inducing the widespread oil shale deposition in Mongolia. |
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| Keywords: |
Cretaceous humid climate
Jurassic lake
Mongolia oil shale
U– Pb age varve |
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