Nandeli Shale Fm
Lithology and Thickness
Shale, siltstone. Composed mainly of sandstone mudstone heterolith, and is characterized by intense soft sediment deformation in several stratigraphic levels. The deformation is manifested by ball and pillow structures, detached sandstone balls enclosed within red shale, or small sand volcano type structures protruding through shale. Many undeformed thin sheets of sandstone exhibits straight crested ripples, interference ripples and rain prints covering large areas of sandstone-pavements. The upper part of the sequence is shale dominated.
Relationships and Distribution
Lower contact
Underlain by Sarnadih Sandstone Fm with gradational contact
Upper contact
Unconformity, overlain by Gondwana Supergroup (which begins with early Permian glacial Talchir Fm)
Regional extent
GeoJSON
Fossils
Age
Depositional setting
Muddy shelf, especially for the upper shale-dominated interval.
Additional Information