Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 9
Early exhumation occurred at higher temperature and lower pressure ( T 650 -
800°C at P 4 - 7 kbar ) during the Miocene . This is the dominant metamorphic
event , which obliterated most of evidence for the earlier , higher pressure event .
3 .
Early exhumation occurred at higher temperature and lower pressure ( T 650 -
800°C at P 4 - 7 kbar ) during the Miocene . This is the dominant metamorphic
event , which obliterated most of evidence for the earlier , higher pressure event .
3 .
Page 190
C14 - analyses : M . Geyh , Lower Saxony State Soil Research Office ; Sampled
by M . Kuhle Sample ( tree trunk ) Sample depth Sample location Sample
environment 813C [ % ] Sampling exposure type no Conv . 14C - age ( before
Stadium ...
C14 - analyses : M . Geyh , Lower Saxony State Soil Research Office ; Sampled
by M . Kuhle Sample ( tree trunk ) Sample depth Sample location Sample
environment 813C [ % ] Sampling exposure type no Conv . 14C - age ( before
Stadium ...
Page 278
(a) Lower age limit Less than a kilometer west-southwest of Muth, the lower parts
of the quartzite sequence forming 150 m high ridges are encountered. Here the
quartzites dip 52°NE. The lower part of the Muth Quartzite is reddish and brown, ...
(a) Lower age limit Less than a kilometer west-southwest of Muth, the lower parts
of the quartzite sequence forming 150 m high ridges are encountered. Here the
quartzites dip 52°NE. The lower part of the Muth Quartzite is reddish and brown, ...
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Contents
Evidence | 1 |
Tectonomagmatic Evolutionary Model of the KuluRampur | 47 |
Tectonic and Geochemical Signifcance of Black Shale | 65 |
Copyright | |
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Common terms and phrases
active Alaknanda Arunachal associated bands basin beds belt biotite Central characterized concentration Crystalline deformation Delhi deposits developed direction drainage Early east eastern elements et al evidence exposed extending fault field Figure folds Formation fractures further Garhwal Geol Geological Glacial glacier gneisses grains granite granitoids Group Himalaya India indicate Indus Kuhle Ladakh Late length Lesser limestone lineaments Lower Main major margin metamorphic moraines mountain nature ND ND normal northern Nummulitic observed occur Pakistan parallel pattern phyllites places plane plate Pleistocene Pradesh present quartzite range region represented resulted river rocks Saklani samples schist sediments sequence shale Siang districts side similar Siyom slide slope southern streams structural studies suggest surface Suture Table tectonic thick thrust Tibet trend unit upper valley values Volcanics western zone