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Titlebook: Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India; G. Dhanunjaya Naidu Book 2012 Springer-Verlag Berlin Heidelberg

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樓主: introspective
11#
發(fā)表于 2025-3-23 10:38:41 | 只看該作者
Nicht klassifizierbar – ACHTUNG0?km. It extends from 72.5°E to 82.5°E longitude and 21.5°N to 24°N latitude and the region is interpreted as collision of the Indian plate with the Eurasian plate and as a suture zone of collision of the Bundelkhand protocontinent to the north and the Dharwar protocontinent to the south.
12#
發(fā)表于 2025-3-23 17:17:16 | 只看該作者
13#
發(fā)表于 2025-3-23 20:46:28 | 只看該作者
Gef??e in malignen und benignen Hauttumorent sites, site layout geometry (grid, profile, random, etc.) and the sequence in which sites are recorded are flexible. Multi-phase surveys are in practice, with the initial phase being experimental or reconnaissance in nature and succeeding phases are designed being used with additional data to get
14#
發(fā)表于 2025-3-23 22:20:29 | 只看該作者
15#
發(fā)表于 2025-3-24 03:03:44 | 只看該作者
Konturen einer analytischen Literaturtheorie° and 78° near a latitude of about 21.2° and crosses different kinds of surface geological features. Majority of the stations cover the region of both Deccan traps and alluvial cover located close to Tapti and Gavligarh faults.
16#
發(fā)表于 2025-3-24 08:19:45 | 只看該作者
https://doi.org/10.1007/978-3-531-91822-8cted 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). The earthquakes associated to it point out to the recent tectonic activity in the region. The NSL zone is believed to mark the boundary betwe
17#
發(fā)表于 2025-3-24 10:57:52 | 只看該作者
G. Dhanunjaya NaiduNominated for a Springer Theses Prize by the National Geophysical Research Institute, Hyderabad, India.The present study provides insight into the subduction/collision history of a seismically signifi
18#
發(fā)表于 2025-3-24 17:38:36 | 只看該作者
19#
發(fā)表于 2025-3-24 21:36:42 | 只看該作者
Introduction,0?km. It extends from 72.5°E to 82.5°E longitude and 21.5°N to 24°N latitude and the region is interpreted as collision of the Indian plate with the Eurasian plate and as a suture zone of collision of the Bundelkhand protocontinent to the north and the Dharwar protocontinent to the south.
20#
發(fā)表于 2025-3-24 23:52:47 | 只看該作者
MT Data Acquisition and Analysis,t sites, site layout geometry (grid, profile, random, etc.) and the sequence in which sites are recorded are flexible. Multi-phase surveys are in practice, with the initial phase being experimental or reconnaissance in nature and succeeding phases are designed being used with additional data to get more detail where needed.
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