Epicontinental Permian-Cretaceous seaways in central India: The debate for the Narmada versus Godavari rifts for the Cretaceous-Tertiary incursion

Kumari, V.; Tandon, S. K.; Kumar, Nithin; Ghatak, Arundhuti

doi:10.1016/j.earscirev.2020.103284

Cited by 24 publications

(12 citation statements)

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“…A recent review of the India seaways based on tectonic history and some fossil groups concluded there was inconclusive evidence the Narmada Seaway existed by the end of the Cretaceous (Kumari et al, 2020). Instead, they proposed the Godavari rift basin as the only inland seaway at this time.…”

Section: J O U R N a L P R E -P R O O F Journal Pre-proofmentioning

confidence: 99%

“…A recent study of ammonites and inoceramids in the Nodular Limestone revealed early, middle and late Turonian deposition (Kumar et al, 2018). These deposits mark the eastward-reach of a sea-level transgression during the Turonian (Tandon, 2000;Tripathi, 2006;Bansal et al, 2020;Kumari et al, 2020) and unconformably overlie the predominantly continental Nimar Sandstone.…”

Section: Introductionmentioning

confidence: 97%

“…The Narmada Basin in India is an intracratonic rift basin of intense interest because of its tectonic history and northward journey after the breakup of Gondwana in the Early Cretaceous ~130 Ma (Tandon, 2000;Chatterjee et al, 2013;Kumari et al, 2020). Madagascar separated from India during the Turonian to Santonian transition and from the Seychelles during the Campanian to early Maastrichtian.…”

Section: Introductionmentioning

confidence: 99%

“…Madagascar separated from India during the Turonian to Santonian transition and from the Seychelles during the Campanian to early Maastrichtian. Highlights of this journey are recorded in the Bagh Group exposed in disconnected outcrops along the edges of the Deccan basalt, and overlie Precambrian rocks from Madhya Pradesh to Gujarat (Tandon, 2000;Tripathi, 2006Tripathi, , 2005Kumari et al, 2020) (Fig. 1).…”

Section: Introductionmentioning

confidence: 99%

“…Sediment deposition in the Narmada Basin occurred in a tectonic graben that was largely controlled by uplift, block faulting, volcanic activity, erosion and sea level transgressions (Biswas 1987;Kumar et al, 1999;Tandon, 2000;Tripathi, 2006;Bansal et al, 2020;review in Kumari et al, 2020). Clues to this history can be found in the Late Cretaceous sediments roughly parallel to the present course of the Narmada River.…”

Section: Introductionmentioning

confidence: 99%

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Section: J O U R N a L P R E -P R O O F Journal Pre-proofmentioning

confidence: 99%