INSITU GEOLOGICAL AND GEOCHEMICAL STUDY OF AN ACTIVE HYDROTHERMAL SITE ON THE NORTH FIJI BASIN RIDGE

被引:19
作者
AUZENDE, JM
URABE, T
BENDEL, V
DEPLUS, C
EISSEN, JP
GRIMAUD, D
HUCHON, P
ISHIBASHI, J
JOSHIMA, M
LAGABRIELLE, Y
MEVEL, C
NAKA, J
RUELLAN, E
TANAKA, T
TANAHASHI, M
机构
[1] GEOL SURVEY JAPAN, TSUKUBA, IBARAKI 305, JAPAN
[2] UNIV BRETAGNE OCCIDENTALE, F-29283 BREST, FRANCE
[3] INST PHYS GLOBE, F-75252 PARIS 05, FRANCE
[4] ORSTOM, NOUMEA, NEW CALEDONIA
[5] ECOLE NORM SUPER, GEOL LAB, F-75251 PARIS 05, FRANCE
[6] UNIV TOKYO, FAC SCI, EARTHQUAKE CHEM LAB, BUNKYO KU, TOKYO 113, JAPAN
[7] UNIV PARIS 06, PETROG LAB, F-75252 PARIS 05, FRANCE
[8] JAPAN MARINE SCI & TECHNOL CTR, YOKOSUKA 237, JAPAN
[9] CNRS, INST GEODYNAM, F-06565 VALBONNE, FRANCE
关键词
D O I
10.1016/0025-3227(91)90106-E
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In June 1989 a diving cruise by the submersible Nautile was carried out on the North Fiji Basin spreading ridge. The objective of the cruise was a geological and geochemical study of the active spreading axis and associated hydrothermal processes. This operation was the third cruise of the French-Japanese Starmer project following the two cruises of the R.V. Kaiyo in 1987 and 1988. Six dives along the spreading axis between 16-degrees-58' and 17-degrees-00S show that the axial graben consists of alternating N15-trending horsts and grabens. Extinct hydrothermal sites have been observed all along the graben. These consist of fossil chimneys, oxide staining and dead shells. At 16-degrees-59'S an active chimney has been discovered and called the "White Lady" because of its almost exclusively anhydrite composition. This chimney expels a peculiar water characterized by low chlorinity and a 285-degrees-C maximum temperature. In the northern extremity of the N15 axis a wide fossil hydrothermal site has been explored and sampled. It is located in an area cut by N15, N140 and N60-trending faults and fissures.
引用
收藏
页码:259 / 269
页数:11
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