Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea

Geochemistry of pore water and associated diagenetic reactions in the diapiric area of Yinggehai Basin, northwestern South China Sea
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南海西北莺歌海盆地底辟地区孔隙水地球化学及成岩反应

DOI:
10.1007/s12583-015-0526-y
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发表时间:
2015-06
影响因子:
3.3
通讯作者:
Li X.S.
Li X.S.
中科院分区:
地球科学3区
文献类型:
--
作者:
Jiang T.;Xie X.N.;Chen H.;Wang Z.F.;Li X.S.

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研究了南海西北部莺歌海盆地底辟区孔隙水地球化学特征,阐明了盆地流体的成因和演化。低矿化度孔隙水存在于海相沉积物中
This study examined the geochemical features of pore water in the diapiric area of the Yinggehai Basin, northwestern South China Sea, and illuminated the origin and evolution of basin fluids. Pore water with low salinity occurs in marine sediments in the
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