Zobrazeno 1 - 10
of 42
pro vyhledávání: '"Rakesh K. Dumka"'
Autor:
Rakesh K. Dumka
Publikováno v:
Quaternary Science Advances, Vol 13, Iss , Pp 100166- (2024)
The western part of the Indian plate, which includes three major paleo-rifts, the Kachchh, Narmada and Cambay basins, is tectonically active and has seen moderate to large earthquakes. Regional stress due to the convergence of the Indo-European plate
Externí odkaz:
https://doaj.org/article/d3f75abb055b417795e4280e458e9262
Autor:
Girish Ch. Kothyari, Rakesh K. Dumka, Khayingshing Luirei, Raj Sunil Kandregula, Ajay Kumar Taloor, Kapil Malik, Achla Joshi, Atul K. Patidar, Uday Bhan
Publikováno v:
Geocarto International, Vol 39, Iss 1 (2024)
AbstractThe Kumaun Himalaya is considered as the most active part of the Central Seismic gap in the Indian Sub-continent. In this paper, we presented active surface deformation rates of the Kumaun region from February 2017 to February 2021 using the
Externí odkaz:
https://doaj.org/article/e96d555aab504750b2581e1083e42715
Publikováno v:
Geodesy and Geodynamics, Vol 13, Iss 3, Pp 254-260 (2022)
The Narmada Son Lineament (NSL) is a major palaeo-rift system and seismically active intra-plate region. In this paper, we processed and analyzed the GPS data from 2009 to 2016 to study the geodynamic characteristics of NSL. The velocities derived fr
Externí odkaz:
https://doaj.org/article/187165d638e14779be11f21e8f735583
Autor:
Donupudi Suribabu, Rakesh K. Dumka, Joydeep Paikray, Girish Ch. Kothyari, Mahesh Thakkar, Kandadai V. Swamy, Ajay K. Taloor, Sandip Prajapati
Publikováno v:
Geodesy and Geodynamics, Vol 13, Iss 3, Pp 247-253 (2022)
After the M7.7 earthquake in 2001, the Kachchh rift basin became the focus of various geological and geophysical researches on the western Indian plate. As an essential technology, the Global Navigation Satellite System (GNSS) has been utilized to st
Externí odkaz:
https://doaj.org/article/b25d3be08f9b42599b9a372cc7833962
Publikováno v:
Geodesy and Geodynamics, Vol 13, Iss 3, Pp 219-229 (2022)
The present study area, Dadra and Nagar Haveli, contains several lineaments and traces of active faults. The various aspect of the geomorphic analysis, i.e., stream length (SL) gradient, hypsometric integral (HI), basin shape (BS), valley floor (VF),
Externí odkaz:
https://doaj.org/article/928b3ab9e1e94a4b8878b080ef8c0038
Autor:
Chirag Jani, Raj Sunil Kandregula, Suraj Bhosale, Anil Chavan, Abhishek Lakhote, Subhash Bhandari, Girish Ch Kothyari, Gaurav Chauhan, Rakesh K. Dumka, D. Suri Babu, Adarsh Thakkar, Ajay Kumar Taloor, Anil Gor, M.G. Thakkar
Publikováno v:
Quaternary Science Advances, Vol 4, Iss , Pp 100034- (2021)
In the present study, we have identified the tectonically active zones along the Island Belt Uplift (IBU), an upthrown block of E-W trending Island Belt Fault (IBF). Major and minor transverse faults have segmented the IBU into four sub-uplifts, viz.
Externí odkaz:
https://doaj.org/article/765309fa88e648f2976e7c80bd4c6aed
Autor:
Rakesh K. Dumka, D. Suribabu, Pratishtha Narain, Girish Ch Kothyari, Ajay Kumar Taloor, Sandip Prajapati
Publikováno v:
Quaternary Science Advances, Vol 4, Iss , Pp 100035- (2021)
The Narmada Son Lineament located in the middle part of the Indian plate is to be considered seismically active part and already experienced six moderate earthquakes in the last century. The geological studies summarize that the reactivation of exist
Externí odkaz:
https://doaj.org/article/42ffd3dff1c6458c8d9a8fc90655a41c
Publikováno v:
Applied Computing and Geosciences, Vol 8, Iss , Pp 100041- (2020)
The accumulation of crustal strain towards the western part of India, especially in the Kachchh Rift basin, is making one of the most seismically active parts of the Indian plate. Several strong to major earthquakes, including the recent 2001 (M7.7)
Externí odkaz:
https://doaj.org/article/39b07d4117714601a2262b96978c538f
Publikováno v:
Acta Geodaetica et Geophysica. 57:639-659
Autor:
Rakesh K. Dumka, Sandip Prajapati, Donupudi SuriBabu, Kandadai V. Swamy, Girish Ch. Kothyari, Kapil Malik
Publikováno v:
Geological Journal. 58:683-699