Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Javid A. Ganai"'
Publikováno v:
Journal of Asian Earth Sciences: X, Vol 9, Iss , Pp 100154- (2023)
The Spiti region, renowned as the Museum of Indian Geology, is a world-famous sedimentary succession containing well-exposed sequences from Neoproterozoic to Cretaceous age. In this study, Triassic siliciclastic sedimentary rocks of the Lilang Superg
Externí odkaz:
https://doaj.org/article/46a3cfee594e4bd8b5d8d748128fd7dc
Publikováno v:
Solid Earth Sciences, Vol 3, Iss 2, Pp 33-49 (2018)
Geochemical and isotopic signatures from Lower Carboniferous Limestone of the Lipak Formation of Spiti region, Tethys Himalaya (for the first time) have been studied for palaeo-climatic reconstruction of the region and to evaluate the influence of te
Externí odkaz:
https://doaj.org/article/b80c0a5754a044b995043504648e9b0d
Publikováno v:
Journal of the Geological Society of India. 98:1189-1198
Publikováno v:
Geological Journal. 57:575-592
Publikováno v:
Journal of Earth System Science. 131
Publikováno v:
Geochemistry. :125981
Autor:
Javid A. Ganai, Shaik A. Rashid
Publikováno v:
International Journal of Earth Sciences. 108:863-883
Due to inaccessibility and tough conditions (high-altitude low-oxygen region) very less information is available about the Indian Tethys Himalayan sequences, particularly geochemical data are scarce. An attempt is made in the present study to evaluat
Publikováno v:
Solid Earth Sciences, Vol 3, Iss 2, Pp 33-49 (2018)
Geochemical and isotopic signatures from Lower Carboniferous Limestone of the Lipak Formation of Spiti region, Tethys Himalaya (for the first time) have been studied for palaeo-climatic reconstruction of the region and to evaluate the influence of te
Autor:
Javid A. Ganai, Shaik A. Rashid
Publikováno v:
Journal of Asian Earth Sciences. 157:371-386
Recently published findings indicate that the Ordovician period has been much more dynamic than previously anticipated thus making this period significant in geological time. The Ordovician of India can best be studied in the Spiti region because the
Publikováno v:
Acta Geochimica. 35:428-436
The geochemical characteristics of two sections—the Permian–Triassic boundary (PTB) Guryul Ravine section, Kashmir Valley, Jammu and Kashmir, India; and the Attargoo section, Spiti Valley, Himachal Pradesh, India—have been studied in the contex