2009
DOI: 10.1007/s12594-009-0135-4
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Upper Callovian-Middle Oxfordian belemnite assemblage from Jara Dome, Western Kachchh

Abstract: Belemnites and ammonites were collected from the Dhosa Oolite beds of Jara Dome in Kachchh. The Dhosa Oolite is an important marker of the Mesozoic sediments exposed in the Kachchh Basin. Nine belemnite species are reported belonging to four genera Belemnopsis, Demubelus, Hibolithes and Conodicoelites. These include Belemnopsis Stoliczka and Conodicoelites cf. abadi Challinor. Besides the belemnites, diagnostic ammonoid fauna are also recorded from the studied section enabling better controlled stratigraphic r… Show more

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Cited by 14 publications
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“…Coordinates: Between 23˚43'N to 23˚45'N and 68˚57'E to 69˚00'E Age: Middle to Upper Jurassic (150 -166 My) This site is rich in geological heritage and uncovers the features of Jara Dome structure (Figure 9 in the lower shale beds exposed at the core of the Jara dome marks the boundary between Jumara and Jhuran formations. The dome is marked by various faults and occurrence of doleritic dyke in the vicinity of the faults as shown on a map (Figure 9(b)) [17].…”
Section: Jara Dome: Lakhapur-jara Section Dayapur Geo-stationmentioning
confidence: 99%
“…Coordinates: Between 23˚43'N to 23˚45'N and 68˚57'E to 69˚00'E Age: Middle to Upper Jurassic (150 -166 My) This site is rich in geological heritage and uncovers the features of Jara Dome structure (Figure 9 in the lower shale beds exposed at the core of the Jara dome marks the boundary between Jumara and Jhuran formations. The dome is marked by various faults and occurrence of doleritic dyke in the vicinity of the faults as shown on a map (Figure 9(b)) [17].…”
Section: Jara Dome: Lakhapur-jara Section Dayapur Geo-stationmentioning
confidence: 99%