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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
【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.
【Key words】 Central Pacific Ocean Line Islands manganese crust phosphorite;
- 【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
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