Journal article

Thermal history of the Krishna-Godavari basin, India: Constraints from apatite fission track thermochronology and organic maturity data

HS Sahu, MJ Raab, BP Kohn, AJW Gleadow, KD Bal

Journal of Asian Earth Sciences | PERGAMON-ELSEVIER SCIENCE LTD | Published : 2013

Abstract

The Krishna-Godavari (KG) basin, a passive margin Late Carboniferous to Holocene basin along the rifted east coast of India, includes the deltaic and inter-deltaic regions of the Krishna and Godavari rivers onshore and extends into the offshore. It is one of India's premier hydrocarbon-bearing basins. In an attempt to better understand the thermal history of the basin, apatite fission track (AFT) data has been obtained from six exploration wells (five onshore and one offshore). AFT thermal history models as well as other thermal indicators e.g. vitrinite reflectance (VR), Rock-Eval Tmax data reveal that the host rocks are currently at their maximum post-depositional temperatures and that any..

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Grants

Funding Acknowledgements

Funding for this research was provided by Australia-India Strategic Research Fund. The University of Melbourne thermochronology laboratory receives infrastructure support under the AuScope Program of NCRIS. We are grateful to The Oil and Natural Gas Corporation, India for providing logistic support, making cores and cuttings available for sampling from various wells and providing well completion reports. The paper benefited from the constructive comments of an anonymous reviewer and Prof. Bor-ming Jahn.