The morphotectonic features of non-transform discontinuity at 11°S and its hydrothermal activity, Central Indian Ridge

DC Field Value Language
dc.date.accessioned 2020-07-15T20:33:30Z -
dc.date.available 2020-07-15T20:33:30Z -
dc.date.created 2020-02-11 -
dc.date.issued 2016-10-11 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/24554 -
dc.description.abstract Korea Institute of Ocean Science and Technology (KIOST) has surveyed the CentralIndian Ridge (CIR) between 17˚S and 7˚S to delineate segment morphotectonics as well asto identify hydrothermal activity. We found not only 4 prominent non-transformdiscontinuities (NTDs) and 11 ocean core complexes (OCCs), but also severalhydrothermal activities within these off-axis structures. Here we report the one of thelargest NTD3-1 and the associated hydrothermalism in the region. The NTD3-1 is 44 kmin length and 10 km in width. Glass watch-shaped basin floor of the NTD is flanked by isclearly defined by 4000 m isobath. The NTD adjoins the linear escarpments that displays> 1000 m high in relief. The escarpments strike at 035°, approximately 45° oblique in aclockwise direction to the orientation of two adjoining ridge segments. The fracture zonebetween segment 3-1 and 3-2 along the off-axis is able to be traced but through-goingtrends thereof are not clear at the terrain that immediately flanks segment 3-1 to east andwest for a distance of approximately 75 km and 30 km, respectively.n-transformdiscontinuities (NTDs) and 11 ocean core complexes (OCCs), but also severalhydrothermal activities within these off-axis structures. Here we report the one of thelargest NTD3-1 and the associated hydrothermalism in the region. The NTD3-1 is 44 kmin length and 10 km in width. Glass watch-shaped basin floor of the NTD is flanked by isclearly defined by 4000 m isobath. The NTD adjoins the linear escarpments that displays> 1000 m high in relief. The escarpments strike at 035°, approximately 45° oblique in aclockwise direction to the orientation of two adjoining ridge segments. The fracture zonebetween segment 3-1 and 3-2 along the off-axis is able to be traced but through-goingtrends thereof are not clear at the terrain that immediately flanks segment 3-1 to east andwest for a distance of approximately 75 km and 30 km, respectively. -
dc.description.uri 1 -
dc.language English -
dc.publisher IMMS -
dc.relation.isPartOf Underwater Mining Institute -
dc.title The morphotectonic features of non-transform discontinuity at 11°S and its hydrothermal activity, Central Indian Ridge -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 2 -
dc.citation.startPage 1 -
dc.citation.title Underwater Mining Institute -
dc.identifier.bibliographicCitation Underwater Mining Institute, pp.1 - 2 -
dc.description.journalClass 1 -
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