The tectonic evolution of the Northwestern Himalaya in eastern Ladakh and Lahul, India

@article{Steck1993TheTE,
  title={The tectonic evolution of the Northwestern Himalaya in eastern Ladakh and Lahul, India},
  author={Albrecht Steck and Laurent Y. Spring and Jean-Claude Vannay and Henri Masson and Hugo Bucher and E. Stutz and Robin Marchant and J.-C. Tieche},
  journal={Geological Society, London, Special Publications},
  year={1993},
  volume={74},
  pages={265 - 276}
}
Abstract Geological studies along a transect across the Himalaya in eastern Ladakh and Lahul provide new insights into the Tertiary structural evolution of this region. The initiation of the Nyimaling-Tsarap Nappe is related to an early phase of underthrusting of India below Asia. In Lahul, an opposite vergent intra-continental underthrusting develops immediately after continental collision (NE-vergent Tandi Syncline and Shikar Beh Nappe). This NE-vergent nappe stack is responsible for the… 

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References

SHOWING 1-10 OF 50 REFERENCES
Geological transect across the Northwestern Himalaya in eastern Ladakh and Lahul (a model for the continental collision of India and Asia)
The detailed geological mapping and structural study of a complete transect across the northwestern Himalaya allow to describe the tectonic evolution of the north Indian continental margin during the
Zanskar shear zone: Northeast-southwest extension within the Higher Himalayas (Ladakh, India)
A complete geologic section through the northwestern Himalayas is well exposed in Ladakh, India. The collision between the Indian shield and the Tibetan platform caused large-scale intracrustal
The closing of Tethys and the tectonics of the Himalaya
Recent geological and geophysical data from southern Tibet allow refinement of models for the closing of southern (Neo-) Tethys and formation of the Himalaya. Shelf sediments of the Indian passive
Nappe tectonics, extension, and metamorphic evolution in the Indian Tethys Himalaya (Higher HImalaya
In the southern part of the Indian Tethys Himalaya between SE Zanskar and NW Lahul, nappe tectonics with transport toward the WSW during the main deformation phase has been ascertained. If the
The structure and stratigraphy of SE Zanskar, Ladakh Himalaya
A field study of over 4 km thickness of Cambro-Ordovician to Cretaceous sediments deposited on the passive margin of northern India has provided significant new data on the thickness, age and
Sedimentary record of the northward flight of India and its collision with Eurasia (Ladakh Himalaya, India)
Abstract— Stratigraphic and petrographic analysis of the Cretaceous to Eocene Tibetan sedimentary succession has allowed us to reinterpret in detail the sequence of events which led to closure of
Tectonic evolution of the India/Eurasia collision zone
Since the collision of India with Eurasia at about 45 Ma in the mid-Eocene, roughly north-south intracontinental convergence has occurred at about 5 cma −1 . This convergence has been accommodated
...
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