Geological and geochemical evolution of forming of kalium-rich brine in Sichuan Basin

Geological and geochemical evolution of forming of kalium-rich brine in Sichuan Basin

<正>1 Introduction Sichuan Basin is basically a salt brine reservoir,large closed and semi-closed artesian sedimentary basin with an area of 200,000 Km2 in southeast China.During the forming and evolution of the basin,it has been affected by

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Veröffentlicht in:Acta geologica Sinica (Beijing) 2017-05, Vol.91 (S1), p.140-141
Hauptverfasser: XU, Zhengqi, YIN, Guan, ZHANG, Chengjiang, CHEN, Xuanrong
Format: Artikel
Sprache:eng
Schlagworte:
Brines
Evolution
Forming
Geochemistry
Geology
Saline water
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Zusammenfassung:<正>1 Introduction Sichuan Basin is basically a salt brine reservoir,large closed and semi-closed artesian sedimentary basin with an area of 200,000 Km2 in southeast China.During the forming and evolution of the basin,it has been affected by
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.13226