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Global Geology 2016, 19(4) 255-276 DOI:
ISSN: 1673-9736 CN: 22-1371/P |
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Episodes of subaerial Large Igneous Provinces (LIPs) linked to late Turonian/late Maastrichtian deep incursion of sea on the Indian continental block |
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Syed A�� Jafar |
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National Centre for Antarctic and Ocean ��esearch (NCAO��) Headland Sada��Vasco-da-Gama��Goa-403804��India |
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Abstract��
Late Cretaceous sea inundation of major continents��surprisingly did not affect Indian block except by two major subaerial events of Large Igneous Provinces (LIPs)�� Marion hotspot induced LIP of Mahajanga Flood Basalt (ca��92 Ma) in Madagascar triggered high intensity earthquake along Narmada Lineament and permitted a short lived marine transgression during late Turonian with spectacular estuarine deposits of limited thickness�� preserved as archive of“Greenhouse Climatic ��ecord”�� ��éunion hotspot induced LIP of Deccan Flood Basalt�� stretching from western to eastern India around ��ajahmundry area attracted worldwide attention for the unique fauna and flora preserved in the intertrappean beds straddling Cretaceous-Palaeogene boundary�� This massive subaerial LIP (ca�� 66Ma) permitted fairly deep penetration of sea along collision facing Subathu-Dogadda Line- ament during late Maastrichtian-Danian��but due to thick vegetation cover��tectonic disturbance and scarce out- crops the evidence is less straightforward than along Narmada rift�� |
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Keywords��
LIPs
marine incursions
Indian Block
late Turonian-Narmada Basin Lineament
Late Maastrici- tian-Subathu Dogadda Lineament
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Received Revised Online: |
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