MASSIVE DEEP-SEA SULFIDE ORE-DEPOSITS DISCOVERED ON THE EAST PACIFIC RISE

被引:279
作者
FRANCHETEAU, J
NEEDHAM, HD
CHOUKROUNE, P
JUTEAU, T
SEGURET, M
BALLARD, RD
FOX, PJ
NORMARK, W
CARRANZA, A
CORDOBA, D
GUERRERO, J
RANGIN, C
BOUGAULT, H
CAMBON, P
HEKINIAN, R
机构
[1] UNIV NACL AUTONOMA MEXICO,INST GEOL,MEXICO CITY 20,MEXICO
[2] WOODS HOLE OCEANOG INST,WOODS HOLE,MA 02543
[3] SUNY ALBANY,ALBANY,NY 12222
[4] UNIV RENNES,GEOL STRUCT LAB,F-35031 RENNES,FRANCE
[5] US GEOL SURVEY,MENLO PK,CA 94025
[6] CTR CIENCIAS MAR & LIMNOL,MEXICO CITY 20,MEXICO
[7] UNIV LOUIS PASTEUR,MINERAL PETROG LAB,F-67084 STRASBOURG,FRANCE
[8] UNIV SCI & TECH LANGUEDOC,GEOL STRUCT LAB,F-34000 MONTPELLIER,FRANCE
[9] UNIV NACL AUTONOMA MEXICO,INST GEOL,MEXICO CITY 20,MEXICO
关键词
D O I
10.1038/277523a0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Massive ore-grade zinc, copper and iron sulphide deposits have been found at the axis of the East Pacific Rise. Although their presence on the deep ocean-floor had been predicted there was no supporting observational evidence. The East Pacific Rise deposits represent a modern analogue of Cyprus-type sulphide ores associated with ophiolitic rocks on land. They contain at least 29% zinc metal and 6% metallic copper. Their discovery will provide a new focus for deep-sea exploration, leading to new assessments of the concentration of metals in the upper layers of the oceanic crust. © 1979 Nature Publishing Group.
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页码:523 / 528
页数:6
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