2023年10月1日 · Narmada-Son Lineament (NSL) is a prominent geo-tectonic feature located in central India, characterised by complex geological structures and evolutionary history. In this study, we present a detailed joint interpretation of the aeromagnetic and gravity anomaly maps to delineate the crustal structure in order to address the thermo-tectonic ...

Central India is traversed by a WSW-ENE trending Narmada-Son lineament (NSL) which is characterized by the presence of numerous hot springs, feeder dykes for Deccan Traps and seismicity all along...

Comprehensive background information and detailed description of magnetotelluric analyses along four traverses across the Son-Narmada-Tapti Lineament, one of the most prominent geomorphic features in the Indian subcontinent with a length of about 1,200 km

2014年6月24日 · Aeromagnetic data analysis over the Narmada-Son Lineament (NSL) shows that prominent anomalies are located over dyke swarms and trap flows and the major formations present have distinct magnetic signatures.

2019年5月22日 · Narmada-Son lineament (NSL) is located on an active intra- continental paleo-rift in the central part of India, and has been reactivated several times in the geological past (Choubey, 1971). The...

In central part of India, Son- Narmada-Tapti (SONATA) is aprominent ENE- WSW trending lineament zone which is bound by two major faults namely Son-Narmada South Fault (SNSF) and Son-Narmada-North Fault (SNNF), reaching upto Moho (Jain et al., 1995). The lineament zone extends about 1300 km from

Three Deep Seismic Sounding (DSS) profiles: (1) Mehmadabad-Billimora, (2) Ujjain-Mahan and (3) Khajuria Kalan-Pulgaon, each about 250 km long were shot by the National Geophysical Research Institute, Hyderabad, India, across the Narmada-Son lineament. This lineament cuts across the whole of central India in a NNE-SSW direction.

1992年2月29日 · The Narmada-Son Lineament (NSL) is a very prominent feature on the tectonic map of India and divides the Indian peninsula into two parts, the northern part characterised by lower elevations and more positive Bouguer gravity anomalies as compared to the southern part.

2012年1月1日 · The Son–Narmada–Tapti lineament zone in central India is the second most important tectonic feature after Himalayas in the Indian geology. It is dissected by several E–W trending faults; the major ones being the Narmada south fault (NSF), Barwani-Sukta fault (BSF), Tapti fault (TF) and Gavilgarh fault (GF).

Geological, geomorphological, geophysical, petrological and mineralisation evidences have been presented to show that the Narmada-Son line is a line of dislocation from Precambrian to Recent times. Maps have been drawn on the basis of available evidence showing the location of …