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Volumn 51, Issue 2, 1998, Pages 245-248

Isotopic evidence of a rapid cooling and continuous sedimentation across the Eocene-Oligocene Boundary of Wagapadhar and Waior, Kutch

Author keywords

Eocene Oligocene boundary; Gujarat; Isotope; Kutch

Indexed keywords

COOLING; EOCENE-OLIGOCENE BOUNDARY; OXYGEN ISOTOPE; PALAEOCLIMATE; SEDIMENTATION;

EID: 0031846720     PISSN: 00167622     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article
Times cited : (8)

References (11)
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  • 2
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  • 3
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    • Kejowin, L.D.1    Corliss, B.H.2
  • 5
    • 0000515442 scopus 로고
    • The zonal distribution of the larger foraminifera of the Eocene of the Western India
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  • 6
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    • The late Eocene-Oligocene extinctions
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  • 8
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    • Pellatispira crassi-culumnata from Kachchh, Gujrat
    • RAY, A.K. and CHAKI, T. (1997). Pellatispira crassi-culumnata from Kachchh, Gujrat. Jour. Geol. Soc. India, v.50, pp.629-632.
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    • Ray, A.K.1    Chaki, T.2
  • 9
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    • Stable isotope studies of fossiliferous Palaeogene sequence of Kutch, Western India; Palaeoenvironmental implications
    • SARKAR, A., RAY, A.K. and BHATTACHARYA, S.K. (1996). Stable isotope studies of fossiliferous Palaeogene sequence of Kutch, Western India; Palaeoenvironmental implications. Palaeogeog. Palaeoclimat. Palaeoecol., v.121, pp.65-77.
    • (1996) Palaeogeog. Palaeoclimat. Palaeoecol. , vol.121 , pp. 65-77
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.