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    西藏定结盆地第四纪湖相地层的厘定、划分和定结群的建立

    The definition and classification of Quaternary Lacustrine strata and the establishment of Dingjie Group in Dingjie basin, Tibet

    • 摘要: 提要:通过对西藏定结盆地湖相沉积的野外地质调查和实测剖面,对分布于盆地内的第四纪湖相地层进行了详细的研究和划分,重新厘定了该区中更新世—晚更新世的岩石地层单元,确立了生物地层和年代地层序列。首次建立了该区第四纪中更新世—晚更新世湖相地层单位——定结群(Qp2-3D)。定结群是由中更新统叶如藏布组(Qp2ly)和上更新统麻加组(Qp3lm)2个组组成。为青藏高原湖泊演化、气候变化、古地理变迁的研究,以及第四纪地层的划分与对比等都提供了新资料。

       

      Abstract: Abstract:Based on the field geological survey and the study of the measured profile of lacustrine sediments in Dingjie basin of Tibet, the authors conducted a detailed study and classification of the Quaternary lacustrine deposits distributed in the basin, redefined the middle Pleistocene–late Pleistocene stratigraphic units and established the sequence of biostratigraphy and lithostratigraphy. The authors have established for the first time the stratigraphic unit of Dingjie Group which belongs to middle Pleistocene–late Pleistocene lacustrine strata. Dingjie Group comprises middle Pleistocene Yeruzangbu Formation and upper Pleistocene Majia Formation. The lacustrine strata provide new material for the study of lake evolution, climate change, palaeogeographic change and division and correlation of Quaternary strata in the Tibetan Plateau.

       

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