Tectonics of the Greater India Proterozoic Fold Belt, with emphasis on the nature of curvature of the belt in west-central India

2021 ◽  
pp. 103758
Author(s):  
Anwesa Banerjee ◽  
Nicole Sequeira ◽  
Abhijit Bhattacharya
Keyword(s):  
2018 ◽  
Vol 52 (2) ◽  
pp. 240-244
Author(s):  
Satish Pande ◽  
Reuven Yosef ◽  
Prashant Deshpande ◽  
Rajkumar Pawar ◽  
Murlidhar N. Mahajan

2021 ◽  
pp. SP515-2020-206
Author(s):  
Prabhin Sukumaran ◽  
Hong-Chun Li ◽  
Jih-Pai Lin ◽  
Parth R. Chauhan

AbstractThe formal beginning of geoarchaeology in India can be traced back to 1863 when the first Palaeolith was documented and collected by Robert Bruce Foote in Tamil Nadu and later described in a detailed geological context. Today, various geological tools such as geospatial analytical tools are available to provide extra mileage to geoarchaeological investigations. They supplement field evidence and enable researchers to display, manipulate, and model geological data and the associated archaeological evidence. The present paper attempts to summarise the current status of understanding the Quaternary geoarchaeology of the Tapi River basin in west-central India. The aspects considered include geomorphology, landform evolution, morphometric parameters, relationships between climate and basin evolution, and Palaeolithic and Mesolithic evidence. This present study uses Landsat imagery, locational data, Survey of India (SOI) topographic sheets and Shuttle Radar Topography Mission (SRTM) data in ArcGIS software. The study is the first comprehensive attempt to summarise the issue of prehistoric human adaptations (dominated mainly by Late Pleistocene evidence) through changing environments, with an assumption that the two occurred in synchronisation. Another assumption is that the reported lithic and fossil sites and the surrounding areas have preserved signatures of original landforms and sedimentary contexts.Through these perspectives and visual integration of topography, drainage networks and Landsat image parameters in a Geographic Information System (GIS) platform, along with other variable field inputs, a testable hypothetical model of the Quaternary evolution of Central Tapi valley is proposed. Additionally, an AMS date of 47,145 cal BP for a newly-discovered ostrich eggshell fragment from Sakegaon near Bhusawal is presented and its palaeoanthropological implications are discussed. Altogether, our observations from the study area, such as an expansion of land use from the Acheulean onwards, signatures of arid phases and the oldest reported ostrich eggshell (OES), warrant further detailed multidisciplinary research. An in-depth understanding of the first-to-last occurrences of ostriches in the region and comprehensive picture of their pan- South Asian distribution, in general, will help address the issue of prehistoric human adaptations through changing environments.


2012 ◽  
Vol 61 (2) ◽  
pp. 156-167
Author(s):  
Mohammad Babar ◽  
Radhakrishna Chunchekar ◽  
Madhusudan G. Yadava ◽  
Bhagwan Ghute

Abstract. Im vorgelegten Artikel werden die Morphostratigraphie, Lithostratigraphie sowie die Sedimentstrukturen des Terna Beckens in der Deccan Basaltic Province (DBP) im westlichen Zentralindien vorgestellt. Die Quartärablagerungen können in drei große Einheiten unterteilt werden (i) dunkelgraue Schluffablagerungen – Spätes Holozän, (ii) hellgraue Schluffablagerungen – Frühes Holozän, (iii) dunkelgrau-braune Schluffablagerungen – Spätpleistozän mit altquartären alluvialen Absätzen mit oberpleistozänen Altern. Die feinen tonig-schluffigen Ablagerungen im Unterlauf des Flusses deuten auf ruhige Ablagerungsbedingungen und einen sinusartigen Abfluss hin. Der Fluss zeigt Tendenzen zu abschwemmungsbedingten Gerinneverlagerungen, die wiederum durch vorhandene Bruchlinien gesteuert wurden. Entlang des Terna-Flusses konnten weiterhin Paläouferrücken in Form von 4–5 m hohen Rücken nachgewiesen werden, hier vor allem im Bereich der OrtschaftenTer, Killari, Sastur, Dhuta und Makni. Einige nachgewiesene Bruchlinien treten vor allem in NE-SE, NW-SE, E-W und WNW-ESE-Richtung auf und bestimmen die Struktur des Grundgebirges im Untersuchungsgebiet. Die TSI-Werte (Topographic Sinousity Index) verdeutlichen einen Erosionswechsel im Untersuchungsgebiet mit einer Verstärkung des topographischen Einflusses auf die Ausformung der Abflussbahnen. Die im Profil sichtbare Geländekante zeugt weiterhin von einer tektonischen Hebung des Gebietes im Quartär. Radiokohlenstoffdatierungen, die an einigen Holzkohlefragmenten durchgeführt wurden, die aus gefalteten Ablagerungen entnommen wurden, deuten darauf hin, dass eine seismische Aktivität in der Zeitspanne zwischen 120–1671 n. Chr. stattgefunden haben kann.


Author(s):  
Parashar Preeti and D. A. Dhale

West Nimaris the South Western region of Madhya Pradesh state in West Central India. The region lies south of the Vindhya Ranges and consists of two portions of the Narmada and Tapti river valleys separated by a section of the Satpurarange. Bhil, Bhilala, Gond, Nayika and Tadwi are dominant tribe of the region. They are dependent on plant based medium and other for recovery of their ailment. The purpose of these studies was to gather ethnoveterinary medicinal knowledge from the area's livestock owners. Traditional healers gathered data on ethnoveterinary medicines through verbal and informal interviews, followed by a well-structured questionnaire. The majority of plants are dicotyledons, with monocotyledons accounting for a small percentage of the total. The leaves are used the most, followed by roots, rhizome, stem, gum, whole plant, and fruits. In the treatment, dermal approaches are used. In many circumstances, plant products, such as sindoor (vermillion), and cow urine, are utilised to treat horn cancer or fractured horn


BMJ ◽  
1968 ◽  
Vol 3 (5621) ◽  
pp. 769-774 ◽  
Author(s):  
P. M. Dalal ◽  
P. M. Shah ◽  
R. R. Aiyar ◽  
B. J. Kikani

2017 ◽  
Vol 18 (2) ◽  
pp. 381-396 ◽  
Author(s):  
Debanjan Sinha ◽  
Tajdarul H. Syed ◽  
James S. Famiglietti ◽  
John T. Reager ◽  
Reis C. Thomas

Abstract Frequent recurrences of drought in India have had major societal, economical, and environmental impacts. While region-specific assessments are abundant, exhaustive appraisal over large spatial scales has been insubstantial. Here a new drought index called Water Storage Deficit Index (WSDI) is devised and analyzed for holistic representation of drought. The crux of the method is the employment of terrestrial water storage (TWS) variations from Gravity Recovery and Climate Experiment (GRACE) for quantification of drought intensity and severity. Drought events in recent times are well identified and quantified using the approach over four homogenous rainfall regions of India over the period from April 2002 to April 2015. Among the four regions, the highest peak deficit of −158.00 mm is observed in January 2015 over central India. While the drought of 2002–04 is prominent in peninsular and west-central India, the drought of 2009–10 and 2012–13 is conspicuous in almost all four regions of India. The longest deficit period of 23 months (from February 2009 to December 2010) and the highest severity value of −26.31 are observed in central and northwestern India, respectively. WSDI values show an increasing trend in west-central India (0.07 yr−1), indicating recovery from previously existing drought conditions. On the contrary, a decreasing trend in WSDI is observed in northwestern (−0.07 yr−1) and central (−0.18 yr−1) India. Results demonstrate considerable confidence in the potential of WSDI for robust characterization of drought over large spatial scales.


2000 ◽  
Vol 8 (4) ◽  
pp. 368-378 ◽  
Author(s):  
H. Kulkarni ◽  
S. B. Deolankar ◽  
A. Lalwani ◽  
B. Joseph ◽  
S. Pawar

2021 ◽  
Vol 7 (1) ◽  
pp. 96-101
Author(s):  
Dhaivat Shah ◽  
Pradeep Ramteke ◽  
Hardik Jain ◽  
Rahul Singh ◽  
Garima Vaishnav

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