The Structural and Tectonic History of India |
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Page 26
Maharajapuram Sitaram Krishnan. therefore be of Middle Jurassic to early Cretaceous age , and in- deed , Cotter ( 1938 , p . 36 ) was of the opinion that the Upper Gondwanas of the East Coast were of Lower Cretaceous age . In the ...
Maharajapuram Sitaram Krishnan. therefore be of Middle Jurassic to early Cretaceous age , and in- deed , Cotter ( 1938 , p . 36 ) was of the opinion that the Upper Gondwanas of the East Coast were of Lower Cretaceous age . In the ...
Page 37
... Cretaceous flysch asso- ciated with the exotic limestone blocks of Permian to Cretaceous ages and basic igneous intrusives and lava flows from the north- east . These exotics and associated rocks do not belong to the Himalayan Tethyan ...
... Cretaceous flysch asso- ciated with the exotic limestone blocks of Permian to Cretaceous ages and basic igneous intrusives and lava flows from the north- east . These exotics and associated rocks do not belong to the Himalayan Tethyan ...
Page 67
Maharajapuram Sitaram Krishnan. 12. Cretaceous Cretaceous strata occupy large areas in the Himalayas and Tibet . In Spiti the Lower Cretaceous is represented by yellow glauconitic sandstones and slaty quartzites called the Giumal ...
Maharajapuram Sitaram Krishnan. 12. Cretaceous Cretaceous strata occupy large areas in the Himalayas and Tibet . In Spiti the Lower Cretaceous is represented by yellow glauconitic sandstones and slaty quartzites called the Giumal ...
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