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- W2390441210 abstract "Palaeocene-Eocene deposited thick gypsum-salt rock layer in Thongmang area which is located in the hinterland of Vientiane basin. Potassium and magnesium salt deposit of Tagong group and overlying clastic rock have a conformable contact. A strip shaped uplift of the salt anticline was formed in Thongmang area because of strong extrusion and difference of overlying weight in middle and late Himalayan movement. The salt tectonic was influenced by many factors in Thongmang region. Difference of overlying weight was the power source of forming salt structure,and rapid settlement of the cap layer was the main reason for slow salt tectonic growth.And strong regional squeezing action accelerated further development of overlying weight differences,gravity and buoyancy.The patterns of salt anticline tectonic are relatively simple which mainly being salt pillow and salt anticline.Research on salt tectonic has great significance for studying the causes of potassium and magnesium salts,tectonization and mineralization." @default.
- W2390441210 created "2016-06-24" @default.
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- W2390441210 date "2009-01-01" @default.
- W2390441210 modified "2023-09-26" @default.
- W2390441210 title "Salt Tectonic Characteristic and Genetic Mechanism of Thongmang Region in Vientiane Basin,Laos" @default.
- W2390441210 hasPublicationYear "2009" @default.
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