<SPAN lang=EN-US style="FONT-SIZE: 14pt; LINE-HEIGHT: 150%"><FONT face="Times New Roman">Sedimentary Facies and Environment Evolution during Devonian to Paleogene in Middle <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on">Kunlun</st1:place> Area<?xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p></o:p></FONT></SPAN>

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LINE-HEIGHT: 150%">Sedimentary Facies and Environment Evolution during Devonian to Paleogene in Middle Kunlun Area

详细信息

责任者：Liu Aimin (Guizhou Academy of Geologic Survey ; Guiyang 550005 ; China) ; Liu Lingyun
刊名：Guizhou Geology
出版年：2009
卷期：18(1)
关键词：沉积相 ; sedimentary facies ; 昆仑山 ; Kunlun Mountains
页码：p.7-12, 6
图表：1 illus., 3 refs.
分类号：0803
issnNo：ISSN1000-5943
isbnNo：CN52-1059/P

摘要

LINE-HEIGHT: 150%">By analyzing the sedimentary characters of middle Kunlun area in different period, it’s thought that Devonian to Paleogene can be divided into two sedimentary environments: continental facies and sea facies. Continental facies mainly distributed in Jurassic to Paleogene, sea facies mainly distributed in Devonian to Triassic formed 5 facies and some sedimentary environments. This area experienced the enlargement of former Tethys Ocean and closed epeirogenetic stage, the formation of south Kunlun Ocean and epeirogenetic stage, the formed and developed stage of foreland basin and the developed stage of mountain and basin continental facies.