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dc.contributor.authorKhadkikar, A.S.
dc.contributor.authorBasavaiah, N.
dc.contributor.authorGundurao, T.K .
dc.contributor.authorRajshekhar, C.
dc.date.accessioned2015-08-25T07:09:27Z
dc.date.accessioned2021-02-12T10:54:26Z-
dc.date.available2015-08-25T07:09:27Z
dc.date.available2021-02-12T10:54:26Z-
dc.date.issued2004
dc.identifier.citationJournal of Indian Geophysical Union, v.8/1, p.49-53, 2004.en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/276-
dc.description.abstractThe palaeogeography and palaeoenvironments around Lothal, a Harappan port town, are reported based on remote sensing, environmental magnetic and Fourier transform infrared spectroscopy studies respectively. The results show that the uppermost part of the sediment record north of Lothal are characterized by low χ fd implying reduced monsoon rainfall. This reduction of monsoon rainfall was accompanied by high sea levels and is comparable with other global sea level and palaeoclimatic records.en_US
dc.language.isoenen_US
dc.subjectPalaeogeographyen_US
dc.subjectMonsoon rainfallen_US
dc.subjectWestern Indiaen_US
dc.subjectEnvironmental magneticen_US
dc.subjectLothalen_US
dc.titlePalaeoenvironments around the Harappan Port of Lothal, Gujarat, western Indiaen_US
dc.typeArticleen_US
dc.identifier.accession090764
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