File:Photomicrographs-of-zeolite-diagenesis-and-dissolved-zeolite-related-to-basalt-eruption-of-the-Paleogene-sandstone-reser.jpg

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English: Photomicrographs of zeolite diagenesis and dissolved zeolite related to basalt eruption of the Paleogene sandstone reservoirs in well BZ-1. (a) Zeolite precipitated perpendicular to basalt rock fragments, E 3 d 1 , 2259 m (7411 ft). (b) Zeolite filled in intergranular pores, E 3 d 1 , 2265 m (7431 ft). (c) Zeolite developed pervasively and chlorite clay envelope occurred, E 3 d, 2351 m (7713 ft). (d) Micrograph of thin section showing the zeolite partly and completely dissolved and chlorite clay envelope occurred, E 3 d 1 , 2280 m (7480 ft). (e) Micrograph of thin section showing dissolved amygdaloid pores of zeolite, E 3 d 1 , 2280 m (7480 ft). (f) Micrograph of thin section showing the zeolite partly and completely dissolved, E 3 d 1 , 2280 m (7480 ft). BR = basalt rock fragments, CCE = chlorite clay envelope, Kf = K-feldspar, Q = quartz, Zeo = zeolite, and ZDP = zeolite dissolved pore.
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Source Zhongheng Sun, Hongtao Zhu, Changgui Xu, Xianghua Yang, Xiaofeng Du, Qingbin Wang, Jinyang Qiao. "Pore Fluid Evolution Influenced by Volcanic Activities and Related Diagenetic Processes in a Rift Basin: Evidence from the Paleogene Medium-Deep Reservoirs of Huanghekou Sag, Bohai Bay Basin, China ," Geofluids doi:10.1155/2017/9732575
Author Zhongheng Sun, Hongtao Zhu, Changgui Xu, Xianghua Yang, Xiaofeng Du, Qingbin Wang, Jinyang Qiao
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current14:47, 12 January 2018Thumbnail for version as of 14:47, 12 January 2018660 × 511 (409 KB)Sohmen (talk | contribs)Transferred from https://www.hindawi.com/journals/GEOFLUIDS/2017/9732575.fig.005a.jpg

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