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中太平洋锰结壳的一种磷块岩基质

A PHOSPHORITE GROUND MASS OF MANGANESE CRUST IN THE CENTRAL PACIFIC OCEAN

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【作者】 单连芳许东禹

【Author】 Shan Lianfang Xu Dongyu(Institute of Marine Geology, MGMR, Qingdao, 266071. China)

【机构】 地质矿产部海洋地质研究所地质矿产部海洋地质研究所 青岛266071青岛266071

【摘要】 在莱恩群岛北端(164°49′W,9°10′N)发现一块作为锰结核基质的磷块岩,含P2O5平均为6.65%。该磷块岩是交代成因的,其形成时代为早始新世以后。

【Abstract】 This paper reported a phosphorite and collophane found in the north end (164°49’W, 9°10’N) of the Line Islands in the Central Pacific Ocean. The phosphorite is ground mass of manganese crust and occurs on the top of a seamount at water depth of 1640m. There is coccolith ooze in association with the crust. The phosphorite is actually a breccia, in which fragments are oli-vine basalt (65% in percentage) and cement is phosphatied impalpable limestone with 19.04% of P2O5. In the phosphorite, P2O5 is about 6.65% on the average. The phosphorite may be formed by the carbonate cement (filler) being replaced by phosphate-bearing pore water.

  • 【文献出处】 海洋地质与第四纪地质 ,Marine Geology & Quaternary Geology , 编辑部邮箱 ,1992年04期
  • 【被引频次】3
  • 【下载频次】28
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