Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 24
... sedimentary attributes recorded against stratigraphic thickness may constitute time series vectors . Since sedimentary deposits are the response to a number of geological processes , a quantitative record of any sedimentary property ...
... sedimentary attributes recorded against stratigraphic thickness may constitute time series vectors . Since sedimentary deposits are the response to a number of geological processes , a quantitative record of any sedimentary property ...
Page 153
... sediments rests with the texture and primary sedimentary structures that are the function of current strength transporting the sediments ( Hjulstrom , 1939 ; Guy et al . , 1966 ; Allen , 1969 ; Miall , 1977 ) . Depending upon its ...
... sediments rests with the texture and primary sedimentary structures that are the function of current strength transporting the sediments ( Hjulstrom , 1939 ; Guy et al . , 1966 ; Allen , 1969 ; Miall , 1977 ) . Depending upon its ...
Page 254
... sediments are the result of in- situ oxidation of the bed rocks in the uplands and of the detritus at the SCALE A SEDIMENTARY STRUCTURE COLOUR depositional LITHOLOGY Cist Sitst V.f.sst Cl congl med sst site penecontemporaneously ...
... sediments are the result of in- situ oxidation of the bed rocks in the uplands and of the detritus at the SCALE A SEDIMENTARY STRUCTURE COLOUR depositional LITHOLOGY Cist Sitst V.f.sst Cl congl med sst site penecontemporaneously ...
Contents
INTRODUCTION | 1 |
STRATIGRAPHY | 9 |
ENERGY SEQUENCE CORRELATION | 23 |
Copyright | |
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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