The server is under maintenance between 08:00 to 12:00 (GMT+08:00), and please visit
later.
We apologize for any inconvenience caused
Restoration method of Ordovician weathering crust paleo-geomorphology of leshan-longnv temple paleohigh and its features in central Sichuan
Author(s): PANG Yanjun, DAI Zongyang, LIU Shanhua, PENG Changyong, FENG Renwei
Pages: 8-
10,15
Year: 2007
Issue:
5
Journal: PETROLEUM GEOLOGY AND ENGINEERING
Keyword: 川中; 奥陶系; 印模法; 古地貌恢复; 古地貌特征;
Abstract: 风化壳古地貌与岩溶储层、古地貌圈闭密切相关.碳酸盐岩风化壳岩溶作用的发展及演化明显受控于当时的古地貌形态,而古地貌又控制着地表和地下岩溶水流的流向,进而控制了碳酸盐岩风化壳岩溶作用带内的孔洞发育.川中乐山-龙女寺古隆起经历加里东到海西期120Ma的风化剥蚀,岩溶作用十分发育,奥陶系储层储集空间均由次生溶蚀改造而成.结合本区地层特征,选取适当的层位用"印模"法进行岩溶古地貌恢复,并划分出岩溶高地、岩溶斜坡和岩溶洼地三种地貌单元及次级单元,分析了各个分区特征.
Citations
No citation found
Related Articles
No related articles found