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Enclosed Extent of the Saline Water and its Constraints on the Sedimentary and Salt Forming Characteristics: A Case Study of the Paleogene Playas in Hoh Xil Basin
Author(s) -
GONG Daxing,
YI Haisheng,
ZHOU Jiayun,
WU ChiHua,
Guoqing Xia
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12279_10
Subject(s) - chinese academy of sciences , sichuan basin , china , geology , paleogene , salt lake , geochemistry , structural basin , geography , mining engineering , archaeology , geomorphology
1 Introduction There is a long period of hot,arid climates in the Jurassic-Neogene,in the eastern of the Neo-Tethys where is been called Western Yunnan—Qiangtang tectonic belt(Zheng et al.,2010).Especially in the Paleogene,under the control of the planetary winds and the north subtropical high pressure belts,a ribbon arid,semi-arid