Petroleum Science >2018, Issue 1: 41-50 DOI: https://doi.org/10.1007/s12182-017-0214-x
Discovery and significance of Quaternary aqueously deposited aeolian sandstones in the Sanhu area, Qaidam Basin, China Open Access
文章信息
作者:Wen-Jing Mao and Shao-Bin Guo
作者单位:
1 School of Energy Resources, China University of Geosciences, Beijing 100083, China; 2 Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, Ministry of Education, Beijing 100083, China and 1 School of Energy Resources, China University of Geosciences, Beijing 100083, China; 2 Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, Ministry of Education, Beijing 100083, China
投稿时间:2017-07-03
引用方式:Mao, WJ. & Guo, SB. Pet. Sci. (2018) 15: 41. https://doi.org/10.1007/s12182-017-0214-x
文章摘要
Influenced by neo-tectonic movement, the Sanhu area of China’s Qaidam Basin formed in the Quaternary in response to migration of its depocentre. A study of core material from the Qijia 1 Well reveals novel Quaternary aqueously deposited aeolian sandstones in the Qigequan Formation of the Sanhu area. Here we report the sedimentary petrology and geochemistry data of these deposits that constrain their depositional history. Evidence for aeolian influence during deposition includes: sorting and roundness, pure quartz sand with single mode grain size distribution and few suspension materials, very fine sand grain size distribution indicating sorting by saltation and suspension transport, dish-shaped and crescentshaped pits in grain surfaces indicating aeolian transport and chemical composition similar to that observed in active or recent dune deposits, namely enrichment in SiO2, Na2O, and MgO relative to the sand dam sediment in the lakeshore. Identification of these aqueously deposited aeolian sandstones expands the range of sedimentary deposit types found in the Sanhu area and improves understanding of its paleoclimatic history.
关键词
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Qaidam Basin, Qigequan Formation, Aqueously deposited, Aeolian sandstones, Paleoclimate