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The Types of Sedimentary Facies and Rock Characteristics of Xujiaweizi Fault Depression in Songliao Basin

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Abstract:

In the Shahezi Formation of Xujiaweizi fault depression in the Songliao Basin mainly tow sedimentary system is developed: the Xudong gentle slope belt and Xuxi fault zone systems. However, this area is little studied as there have been only limited efforts in exploration. Based on the latest drilling, outcrop data, description of core observation and laboratory microscope identification, it has been concluded that four mainly sedimentary facies are developed in this area: braided river delta, fan delta, lacustrine facies and sublacustrine fan. The subaqueous distribute channel is the main type of the fan delta front while the braided channel is the main type of the braided river delta. A number of clastic, sandstone and mudstone are developed in these two types of sedimentary facies. We can use it to make further study of dividing into micro-facies.

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Periodical:

Advanced Materials Research (Volume 787)

Pages:

717-720

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.787.717

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Online since:

September 2013

Authors:

Cheng Zhi Liu, Xue Du, Xiao Zhou, Bo Li, Xi Liu

Keywords:

Core Description, Sedimentary Facies, Sedimentary Micro-Facies, Xujiaweizi Fault Depression

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© 2013 Trans Tech Publications Ltd. All Rights Reserved

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