Low-Temperature Clay Mineral Dehydration Contributes to Porewater Dilution in Bering Sea Slope Subseafloor

Widespread diagenesis of clay minerals occurs in deeply buried marine sediments under high-temperature and high-pressure conditions. For example, the smectite-to-illite (S-I) transformation has been often observed in sediments at in situ temperatures above ~60°C. However, it remains largely unknown...

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Principais autores:	Akira Ijiri, Naotaka Tomioka, Shigeyuki Wakaki, Harue Masuda, Katsumi Shozugawa, Sunghan Kim, Boo-Keun Khim, Masafumi Murayama, Motoyuki Matsuo, Fumio Inagaki
格式:	Artigo
语言:	Inglês
出版:	Frontiers Media S.A. 2018-04-01
丛编:	Frontiers in Earth Science
主题:	smectite-to-illite transformation porewater chemistry clay mineralogy iron reduction Bering Sea Slope
在线阅读:	http://journal.frontiersin.org/article/10.3389/feart.2018.00036/full
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