Tethys Himalaya of Karnali–Bheri Region (Dolpa) | SpringerLink
网页2015年1月1日 · It can be homotaxial with the well-studied Siringothyris Limestone of Kashmir or the Lipak Formation of Spiti, in the Northwest Himalaya (Fuchs 1967). This formation pinches out towards the northwest, and is missing in the western part of the Dolpa Synclinorium (Fuchs 1967, 1974).
Stratigraphy and sedimentary history of the Nepal Tethys Himalaya ...
网页1999年10月1日 · These passive margin sediments are widely exposed in the Dolpo-Manang Synclinorium of northern central Nepal (Fig. 1), where they have been extensively studied by European geologic teams since the early sixties (e.g. Bodenhausen et al., 1964, Fuchs, 1964, Bordet et al., 1964).
Transition from diagenesis to metamorphism in the Paleozoic to …
网页Transition from diagenesis to metamorphism in the Paleozoic to Mesozoic succession of the Dolpo-Manang Synclinorium and Thakkhola Graben (Nepal Tethys Himalaya) | CiNii Research. 【Updated on July 2, 2024】 Integration of CiNii Dissertations and CiNii Books into CiNii Research.
Geological Evolution of the Tethys Himalaya - Himalaya, …
网页2023年7月21日 · The Tethys Himalaya (TH), also known as “Tibetan Zone”, is one of the major tectonic domains within the Himalayan orogen, stretching for approximately 2,000 km from Kashmir and the Zanskar–Spiti synclinorium to South Tibet.
网页Fig. I. -'Geological sketch map of the Dolpo-ManangSynclinorium (compiled after Fuchs, 1977; Bordet et al., 1971; 1975; Colchen et al., 1986; Fuchs et al., 1988). Inset shows distribution of Tethys Himalaya passive margin sediments in the Himalayan Chain. MCT : Main Central Thrust; NF : High Himalaya Normal Fault.
Geological Evolution of the Tethys Himalaya - ResearchGate
网页2023年7月21日 · Deformation of the Tethys Himalaya will be described in two different key areas of the belt, Dolpo (Western Nepal) and Ladakh (NW India), where the sequence offers very good outcrops and ...
The Tethys Himalayan passive margin from Late Triassic to Early ...
网页The Mesozoic sedimentary succession of the Tethys Himalayan Zone has been studied extensively in the last 20 years in the Spiti-Zanskar Synclinorium of Northern India (e.g. Srikantia, 1981; Baud et al., 1982 1984; Fuchs, 1982a,b; Bassoullet et al., 1983; Gaetani et al., 1986; Bhargava, 1987; Bagati, 1990; Gaetani and Garzanti, 1991) and in the ...
Transition from diagenesis to metamorphism in the Paleozoic to …
网页Transition from diagenesis to metamorphism in the Paleozoic to Mesozoic succession of the Dolpo-Manang Synclinorium and Thakkhola Graben (Nepal Tethys Himalaya)
Late Paleozoic and Triassic bryozoans from the Tethys Himalaya …
网页2006年2月1日 · The studied bryozoans were framed in a solid lithostratigraphic scheme spanning across the Tethys Himalaya for over 1500 km, from NW India (Zanskar and Spiti) through Nepal (Dolpo and Manang) to South Tibet; they are concentrated in correlatable stratigraphic intervals corresponding to the Upper …
Transition from diagenesis to metamorphism in the Paleozoic to …
网页New findings of Late Paleozoic and Triassic bryozoans from the Tethys Himalaya are reported. Fifteen species, including three undetermined, were described, while determinations at order, family or …
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