兰州盆地下白垩统碎屑岩层序地层序列:祁连山早白垩世隆升的沉积学响应

doi:10.13278/j.cnki.jjuese.201602102

Abstract

Abstract:

Controlled by the uplift of Qilian Mountains and the change of climate, a set of clastic rocks are developed in Early Cretaceous in the continental basins in front of Qilian Mountains. The Cretaceous strata are developed and outcropped well in Lanzhou basin, which are made up of particular sedimentary facies successions under the framework of the unconventional system tracts, and are very important to the study of the Qilian Mountains uplift and their impacts on the Asian environment. The Lower Cretaceous Hekou Group can be divided into 5 third-order sequences (S.1-S.5), and every third-order sequence contains LAST and HAST unconventional systems. Alluvial fan facies and fluvial facies coarse clastic rocks constitute the LAST;while the HAST is composed by alluvial fan facies. The eolian sandstones in the Upper Part of Hekou Group are the products of "foehn effect" caused by the Qilian Mountains uplift. In the transition period of Early to Late Cretaceous, Qilian Mountains uplifted fast and intensively, which caused the denuded zone of the study area;so the Upper Cretaceous strata were not developed. The Lower Cretaceous sequences of Lanzhou basin are the material records of not only the Qilian Mountains uplift, but also the reconstruction of the pattern of the atmospheric circle in East Asia.

Key words: uplift of Qilian Mountains, Cretaceous, sequence stratigraphy, response of sedimentary, Lanzhou basin

CLC Number:

P544.4

Guo Rongtao, Zhao Xi, Liu Hongguang, Shi Kaibo, Liu Jing, Jiang Qicai. Sequence Stratigraphic Succession of the Lower Cretaceous Clastic Rock System in Lanzhou Basin: Sedimentological Response to the Early Cretaceous Uplift of Qilian Mountains[J].Journal of Jilin University(Earth Science Edition), 2016, 46(2): 321-335.

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Sequence Stratigraphic Succession of the Lower Cretaceous Clastic Rock System in Lanzhou Basin: Sedimentological Response to the Early Cretaceous Uplift of Qilian Mountains

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