Basalt microlapilli in deep sea sediments of Indian Ocean in the vicinity of Vityaz fracture zone
DRS at CSIR-National Institute of Oceanography
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Title |
Basalt microlapilli in deep sea sediments of Indian Ocean in the vicinity of Vityaz fracture zone
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Creator |
Nath, B.N.
Iyer, S.D. |
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Subject |
Geology and Geophysics
quaternary volcanic rocks mid-ocean ridges cores fracture zones sediments basalts ISW, Indian Ocean |
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Description |
Two cores recovered from the flanks of Mid-India oceanic ridge in the vicinity of Vityaz fracture zone consist of discrete pyroclastic layers at various depths. These layers are composed of coarse-grained, angular basaltic microlapilli in which labradorite is the major mineral set in a glassy mesostasis. Chemically the microlapilli are similar to Mid-Indian oceanic ridge basalts. The microlapilli are suggested to have been formed by the process of granulation, transportation and deposition, during Late Quaternary when lava of low viscosity erupted from small vents on a segment of Vityaz fracture zone
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Date |
1995-06-24T10:01:49Z
2017-09-30T01:29:53Z 1995-06-24T10:01:49Z 2017-09-30T01:29:53Z 1989 |
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Type |
Journal Article
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Identifier |
Journal of the Geological Society of India, vol.34; 1989; 303-309
0016-7622 http://drs.nio.org/drs/handle/2264/7149 |
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Language |
en
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Relation |
J Geol Soc India
SCI |
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Publisher |
Geological Society of India
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