Himalaya: Geological Aspects, Volume 4Contributed articles. |
From inside the book
Results 1-3 of 18
Page 84
Early euhedral to late anhedral ( interstitial ) biotite grains noted in ME are
identical to those crystallized in CG but their grain sizes differ markedly . Early
biotite seems to crystallized cotectically with plagioclase , and can be
distinguished from ...
Early euhedral to late anhedral ( interstitial ) biotite grains noted in ME are
identical to those crystallized in CG but their grain sizes differ markedly . Early
biotite seems to crystallized cotectically with plagioclase , and can be
distinguished from ...
Page 279
The lower member comprises mainly coarse , poorly sorted , calcareous
sandstones having high angularity of the framework grains . The proportion of
matrix is relatively high . The middle member contains coarse , moderately sorted
...
The lower member comprises mainly coarse , poorly sorted , calcareous
sandstones having high angularity of the framework grains . The proportion of
matrix is relatively high . The middle member contains coarse , moderately sorted
...
Page 331
Zircon grains from sample 2801 were separated using standard mineral
separation techniques . The grains were then mounted in epoxy resin produced
by mixing Epirez Hardener and Compound , together with chips of the TEMORA
standard ...
Zircon grains from sample 2801 were separated using standard mineral
separation techniques . The grains were then mounted in epoxy resin produced
by mixing Epirez Hardener and Compound , together with chips of the TEMORA
standard ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Evidence | 1 |
Tectonomagmatic Evolutionary Model of the KuluRampur | 47 |
Tectonic and Geochemical Signifcance of Black Shale | 65 |
Copyright | |
13 other sections not shown
Other editions - View all
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