Magnetic anomalies across the southern Central Indian Ridge: evidence for a new transform fault

dc.contributor.author Chaubey, A. K.
dc.contributor.author Krishna, K. S.
dc.contributor.author Subba Raju, L. V.
dc.contributor.author Gopala Rao, D.
dc.date.accessioned 2022-03-26T23:49:39Z
dc.date.available 2022-03-26T23:49:39Z
dc.date.issued 1990-01-01
dc.description.abstract Bathymetric and magnetic studies along seven northeast-southwest profiles across the Central Indian Ridge segment between latitudes 18 and 22°S and longitudes 66 and 69°E reveal a northwest-southeast trending median valley, associated with a broad and high-amplitude magnetic anomaly (the central anomaly) along the ridge crest. A series of linear magnetic anomalies parallel to the ridge are identified as sea-floor spreading lineations 2,2A,3,3A and 4. A half spreading rate of 2.2 cm y-1 is estimated for the last 10 Ma. The ridge jump between the anomalies 2-2A (approx. 2.5 Ma) and a new left lateral transform fault offsetting the ridge axis about 50 km are indicated to explain the magnetic pattern. © 1990.
dc.identifier.citation Deep Sea Research Part A, Oceanographic Research Papers. v.37(4)
dc.identifier.issn 01980149
dc.identifier.uri 10.1016/0198-0149(90)90095-D
dc.identifier.uri https://www.sciencedirect.com/science/article/abs/pii/019801499090095D
dc.identifier.uri https://dspace.uohyd.ac.in/handle/1/2528
dc.title Magnetic anomalies across the southern Central Indian Ridge: evidence for a new transform fault
dc.type Journal. Article
dspace.entity.type
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