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  • The Gongba conglomerates : glacial or tectonic? in Quaternary of the Karakoram and Himalaya.
  • Tibet and north of the Himalayan Range. Rather, these conglomerate beds represent a direct sedimentary response both to the uplift of the Himalayan Range and to the extensional tectonics which have taken place since Plio-Pleistocene times and which
  • Stratigraphic and petrographic study of foredeep molasse sediments, which provide a detrital record of the evolution of the southern Himalayas during the tectonic collision of central Asia and India.
  • the resulting landscapes. This complicates the interpretation of Quaternary tectonic and climatic history. The A. tries to clarify the succession of the glaciations and presents a critical summary and review of the Chinese work.
  • No simple relationship exists between terrace heights, degree of incision and terrace deformation, and the tectonic and climatic history of the area. Allocyclic processes further complicate the interpretation of terrace formation. Six main types