Discovery and significance of Quaternary aqueously deposited aeolian sandstones in the Sanhu area, Qaidam Basin, China
Abstract 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 Sa...
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Formato: | article |
Lenguaje: | EN |
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KeAi Communications Co., Ltd.
2018
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Acceso en línea: | https://doaj.org/article/7842ac69c6714abcb28d1fc28faf281d |
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