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Volumn 33, Issue 5, 2006, Pages 1005-1012

Features of the change in Pliocene depositional environment at the Guge Formation section in the Zanda basin, Tibet

Author keywords

Depositional environment; Guge Formation; Tibet; Zanda basin

Indexed keywords

DEPOSITIONAL ENVIRONMENT; ENVIRONMENTAL CHANGE; LACUSTRINE DEPOSIT; LACUSTRINE ENVIRONMENT; PALEOCLIMATE; PALEOENVIRONMENT; PLIOCENE;

EID: 33846333462     PISSN: 10003657     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article
Times cited : (6)

References (10)
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  • 3
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    • Qian, F.1
  • 5
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    • Quaternary glaciogelogy at the southeastern foot of the Nyainqentanglha Range
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    • Qian Fang, Pu Qingyu, Wu Xihao. Quaternary glaciogelogy at the southeastern foot of the Nyainqentanglha Range [A]. In: Contributions to the Geology of the Qinghai-Xizang (Tibet) Plateau (4)[C]. Beijing. Geological Publishing House, 1982.34-50(in Chinese).
    • (1982) Contributions to the Geology of the Qinghai-Xizang (Tibet) Plateau (4) , pp. 34-50
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    • Zhu Dagang, Meng Xian'gang, Shao Zhaogang, et al, Features of Pliocene -lower Pleistocene sedimentary facies and tectonic evolution in the Zanda basin, Ngari area, Tibet [J]. Journal of Geomechanics, 2004,10(3):245-252 (in Chinese with English abstract).
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  • 7
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    • Discovery of two unconformities in Pliocene -early Pleistocene fluvio - Lacustrine deposits in the Zanda basin, Ngari, Tibet
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.