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Phillipsite in deep-sea sediments
作者姓名:Peng Hanchang  Liu Zhengkun
作者单位:First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China;Institute of Hunan Nonferrous Metals, Changsha 410007, China
基金项目:This project is supported by the National Natural Science Foundation of China.
摘    要:Phillipsiteindeep-seasediments¥PengHanchangandLiuZhengkun(ReceivedMarch5,1993;acceptedAugust14,1993)Abstract:──Aphillipsiteas...

关 键 词:Phillipsite  cross-shaped  twin  authigenous  mineral  volcanic  glass
收稿时间:3/5/1993 12:00:00 AM
修稿时间:1993/8/14 0:00:00

Phillipsite in deep-sea sediments
Peng Hanchang,Liu Zhengkun.Phillipsite in deep-sea sediments[J].Acta Oceanologica Sinica,1994,13(1):107-115.
Authors:Peng Hanchang and Liu Zhengkun
Institution:1.First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China2.Institute of Hunan Nonferrous Metals, Changsha 410007, China
Abstract:A phillipsite as one of oceanic authigenic zeolites gradually forms from alteration of volcanic glass under low temperature and pressure. In this paper physical property and chemical and mineralogical compositions ofsome zeolite grains collected from the study area in the North Pacific Ocean are first comprehensively studied, andthey are defined as phillipsite. Then, statistics of grain percentage of the phillipsite widely-distributed at 35 sitesin the study area in the deep-sea sediments were made ; it has been found that they mainly occur in the two sediments: red clay and calcareous ooze, and are rich in the former. Finally, the authors preliminarily discuss the formation process of the phillipsite on the basis of this study results, together with the view points of predecessors.
Keywords:Phillipsite  cross-shaped twin  authigenous mineral  volcanic glass
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