The Structural and Tectonic History of India |
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Page 18
... Mesozoic and perhaps even early Palaeozoic rocks . It is some fifty miles broad , most of the surface being occupied by Murree ( Oligo - Miocene ) and Siwalik ( Mio - Pliocene ) rocks . Eocene formations as well as Mesozoic and earlier ...
... Mesozoic and perhaps even early Palaeozoic rocks . It is some fifty miles broad , most of the surface being occupied by Murree ( Oligo - Miocene ) and Siwalik ( Mio - Pliocene ) rocks . Eocene formations as well as Mesozoic and earlier ...
Page 37
... Mesozoic age . Still further north is the Darchen zone of flysch with associated igneous rocks and limestone blocks which might possibly represent the root zone of the Kumaon exotics men- tioned above . But the Darchen rocks are thrust ...
... Mesozoic age . Still further north is the Darchen zone of flysch with associated igneous rocks and limestone blocks which might possibly represent the root zone of the Kumaon exotics men- tioned above . But the Darchen rocks are thrust ...
Page 40
... Mesozoic rocks intruded into by Pre - Cambrian and Mesozoic ( presumably Jurassic ) granites . This granite belt passes through Bhamo and Mogok in the north and through Tenasserim into the Malay States in the south . It then turns east ...
... Mesozoic rocks intruded into by Pre - Cambrian and Mesozoic ( presumably Jurassic ) granites . This granite belt passes through Bhamo and Mogok in the north and through Tenasserim into the Malay States in the south . It then turns east ...
Contents
INTRODUCTION | 1 |
THE EXTRAPENINSULAR REGION | 27 |
The Himalayan Arc the Burmese Arc the Baluchistan | 75 |
6 other sections not shown
Common terms and phrases
Africa anomalies appear Arabia Aravalli Assam associated Auden Baluchistan basic basin beds belt border Burma Burmese Central closely coast connected containing continued Cretaceous Cutch deposits developed direction east Eastern Ghats Eocene extended facies faulted fauna flows folding followed formations formed fossils further Garhwal Geol geological geosyncline Gondwanas granite Hills Himalayas India indicate intrusives Iran islands Jurassic Kashmir known later lavas limestones Lower Madagascar marine marked mass Mesozoic Middle miles Miocene mountain movements Mysore Neocomian northern occupied occur original orogeny parallel Peninsula period Permian places plateau Pleistocene Pre-Cambrian present probably Range region represented ridge rift rocks Salt Range sandstones Satpura sediments seen separated shales shallow shows side similar southern strata strike structure Surv Tertiary Tethyan thrust transgression Traps trend Triassic trough ultrabasic uplift Upper Upper Cretaceous Valley Vindhyans volcanic wedge western zone