Godhara Fm
Type Locality and Naming
SUBSURFACE. Interval 850-2049m in well SP-1-1. [Original Publication: Zutshi, P.L., Mittal, S.K and Shah, L. (1993) Lithostratigraphy of Indian Petroliferous Basins, Document IV, Kutch Saurashtra Basin, KDMIPE, ONGC Publication, pp 1-50.]
[Fig. Geological and structural map of Kutch, also showing the onshore and offshore wells drilled for oil exploration. (Map by Rasoul Sorkhabi in GeoExpro Dec2014, based on various sources including S.K. Biswas, Current Science, 25May2005)]
Lithology and Thickness
Shallow-marine marl. It consists of shale/claystone/limestone alternations and minor sandstones. 1200 m in well SP-1-1, thickness increases towards west.
[Figure 1: Seismic section showing Middle Miocene, Early Eocene and Paleocene plays (after Bhowmick and Vasudevan, 2013)]
Relationships and Distribution
Lower contact
Unconformable with the Narayan Sarovar Fm (?; next older subsurface unit seems to be the Mit Nadi Fm). It is marked by sharp break in resistivity and gamma rays logs. It also coincides with the top of M. complanata.
Upper contact
Conformable with the overlying Chassara Fm. It is marked at the end of limestone/claystone alternations to dominantly final clastic of Chassara Fm.
Regional extent
GeoJSON
Fossils
Miogypsina (Miogypsinoides) dehaarti, M (L) excentrica, M. tani, M.(L) thecideaeformis
Age
Depositional setting
Deposited in inner shelf environment
Additional Information