Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 55
... climate , particularly the global climate is , on the. 3 10 2 9 > 7 ) but acidic waters ( pH < 7 ) are detrimental to their stability . The pH of continental waters is largely a function of ambient climate . Continental water is slightly ...
... climate , particularly the global climate is , on the. 3 10 2 9 > 7 ) but acidic waters ( pH < 7 ) are detrimental to their stability . The pH of continental waters is largely a function of ambient climate . Continental water is slightly ...
Page 255
... climate while the red colour signifies oxidation under warm climate . SEDIMENTARY RECORD OF COOLING AND WARMING EPISODES AND GLOBAL CLIMATIC CYCLES Cenozoic sedimentation in the Himalayan foreland basin started under a hot , arid climate ...
... climate while the red colour signifies oxidation under warm climate . SEDIMENTARY RECORD OF COOLING AND WARMING EPISODES AND GLOBAL CLIMATIC CYCLES Cenozoic sedimentation in the Himalayan foreland basin started under a hot , arid climate ...
Page 268
... climate are basically two independent factors . The " hen - egg " comparison between tectonism and climate ( Molnar and England , 1990 ) is not the real question because the former is endogenic to the planet Earth while global climate ...
... climate are basically two independent factors . The " hen - egg " comparison between tectonism and climate ( Molnar and England , 1990 ) is not the real question because the former is endogenic to the planet Earth while global climate ...
Contents
INTRODUCTION | 1 |
STRATIGRAPHY | 9 |
ENERGY SEQUENCE CORRELATION | 23 |
Copyright | |
23 other sections not shown
Common terms and phrases
Anticline autochthon basement Batwan Enseq Beas Beas River Cenozoic Chenab Chimnun cis-garnet clastics claystone climate colour conglomerates cycle Dagshai Dehradun deposits Dharmpur Enseq Dharmsala energy sequence classification Enseq Eocene facies fold belt foothills foreland basin Formation fossils frequency Gandak Ganga GARNET Geol geological cross section grain size trend gravels grey heavy minerals Himalaya India Indo-Gangetic Foredeep Jammu Jawalamukhi Jawalamukhi Enseq Kalidhar Enseq Kangra Kangra Depression Kasauli Khad Kumar Kumarhatti Enseq Lesser Himalaya limestone Lithology location in Fig Makreri Enseq Middle Siwalik Miocene Murree opaque orogenic parautochthon pebble composition Pleistocene Potwar PRE-TERTIARY PT PT quartzite Raiverman Ravi red beds Ridge River Sadhot Enseq sandbodies sandstones Sarda Enseq Sarkaghat sector sedimentary sediments seismic profiles shale shows siltstone Siwalik smectite stratification stratigraphic strike-slip structural Sub-Himalaya Subathu Subathu Depression Syncline tectonic Tertiary Tethyan thickness Tibet traverse trend curve unconformity uplift Upper Siwalik Wah Devi Enseq wrench fault zone