收稿日期: 2012-07-20
修回日期: 2012-09-15
网络出版日期: 2012-10-10
Sedimentary Genetic Types of Coarse Fragment of Paleogene Lulehe Formation in Qaidam Basin and Time Limit of the Tibetan Plateau Uplift
Received date: 2012-07-20
Revised date: 2012-09-15
Online published: 2012-10-10
付玲,关平,简星,刘瑞娟,冯帆,安群,范朝峰 . 柴达木盆地路乐河组粗碎屑沉积成因与青藏高原隆升时限[J]. 天然气地球科学, 2012 , 23(5) : 833 -840 . DOI: 10.11764/j.issn.1672-1926.2012.05.833
In this study,rock assemblage were interpreted credibly in various aspects,including lithological association,sedimentary facies,well logging and geophysical prospecting,on the basis of outcrops,core drilling and seismic data.The results of Paleogene study in Qaidam basin indicate that the coarse clastic sediments in the lower segment of Lulehe Formation have a nearby source and make typical alluvial fans under the oxidation environment.The Mesozoic strata or Paleozoic rocks are defined by an angular unconformity which is overlain by the segment of Lulehe Formation.Basin comprehensive analysis shows Qaidam basin experienced a large-scale intense tectonic movement at the turn of the Cretaceous and the Paleogene.And the sediment records of Lulehe Formation is the response of the collision between India and Eurasian plates.
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