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[HTML][HTML] Triggering mechanism and brittle-ductile dynamics of active faults in the south-central Saurashtra horst, Gujarat, western India: A geospatial, geological, and …
The seismically active Saurashtra horst is located within the intraplate volcanic continental
margin of western India. The region is prone to moderate and low-magnitude earthquakes …
margin of western India. The region is prone to moderate and low-magnitude earthquakes …
Crust beneath the northwestern Deccan Volcanic Province, India: Evidence for uplift and magmatic underplating
Abstract The northwestern Deccan Volcanic Province of India and its pericratonic rift basins
were reactivated during different stages after the breakup of India from the Gondwanaland …
were reactivated during different stages after the breakup of India from the Gondwanaland …
Seismic imprints of plume‐lithosphere interaction beneath the northwestern Deccan Volcanic Province
The interaction of the Indian continental lithosphere with the Reunion plume resulted in
massive outpouring of basalts manifested in the Deccan Volcanic Province. Although it is …
massive outpouring of basalts manifested in the Deccan Volcanic Province. Although it is …
Some geodynamic aspects of Kutch basin and seismicity: An insight from gravity studies
DV Chandrasekhar, DC Mishra - Current Science, 2002 - JSTOR
The Bouguer anomaly of Kutch shows several gravity highs and lows, primarily attributed to
fault-controlled basement uplifts and depressions. Gravity modelling suggests larger …
fault-controlled basement uplifts and depressions. Gravity modelling suggests larger …
The 2007 Talala, Saurashtra, western India earthquake sequence: tectonic implications and seismicity triggering
A damaging and widely felt moderate (Mw 5.0) earthquake occurred in the Talala region of
Saurashtra, Gujarat (western India) on November 6, 2007. The highly productive sequence …
Saurashtra, Gujarat (western India) on November 6, 2007. The highly productive sequence …
Gravity and magnetic signatures of volcanic plugs related to Deccan volcanism in Saurashtra, India and their physical and geochemical properties
DV Chandrasekhar, DC Mishra, GVSP Rao… - Earth and Planetary …, 2002 - Elsevier
The Bouguer anomaly and the total intensity magnetic maps of Saurashtra have delineated
six circular gravity highs and magnetic anomalies of 40–60 mGal (10− 5m/s2) and 800 …
six circular gravity highs and magnetic anomalies of 40–60 mGal (10− 5m/s2) and 800 …
The seismic structure of the Saurashtra crust in northwest India and its relationship with the Reunion Plume
G Surya Prakasa Rao, HC Tewari - Geophysical Journal …, 2005 - academic.oup.com
Summary The Saurashtra Peninsula in northwest India, lying at the northern boundary of the
Deccan Volcanic Province, is almost entirely covered by these volcanics. Analogue seismic …
Deccan Volcanic Province, is almost entirely covered by these volcanics. Analogue seismic …
Geomorphic response to neotectonic instability in the Deccan volcanic province, Shetrunji River, western India: Insights from quantitative geomorphology
T Solanki, PM Solanki, N Makwana, S Prizomwala… - Quaternary …, 2021 - Elsevier
Abstract The Saurashtra peninsula, a Deccan Trap terrain, in western India lacks the studies
that document on-land information of tectonically active faults. In the present paper, the …
that document on-land information of tectonically active faults. In the present paper, the …
Identification of crustal deformation in the Saurashtra region, western India: insights from PSI and GNSS derived investigation
Abstract The Persistent Scatterer Interferometry (PSI) and Global Navigation Satellite System
(GNSS) techniques were used to identify the deformation rates in the Saurashtra region …
(GNSS) techniques were used to identify the deformation rates in the Saurashtra region …
Origin of silicic rocks of the Deccan traps continental flood basalt province: inferences from field observations, petrography, and geochemistry
The origin of silicic rocks (SiO 2> 65 wt%) in Continental Flood Basalt (CFB) provinces could
be attributed to complex petrogenetic processes. The 65.5–66 Ma old Deccan Traps CFB …
be attributed to complex petrogenetic processes. The 65.5–66 Ma old Deccan Traps CFB …