Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
From inside the book
Results 1-3 of 21
Page 54
From the topography , this amount of offset is a maximum estimate and could be
only 2 or 3 km . In any case , if the graben formed at roughly 2 Ma , this 7.5 km
offset cannot be older . The graben is much clearer south of this intersection than
...
From the topography , this amount of offset is a maximum estimate and could be
only 2 or 3 km . In any case , if the graben formed at roughly 2 Ma , this 7.5 km
offset cannot be older . The graben is much clearer south of this intersection than
...
Page 64
EOffset of Pre - Silurian Amphibolite 12.9-13.8 km Offset of Western Limit of Pre -
Silurian Marble 14.5-14.8 km Offset of Oligocene Unconformity 14.0-14.1 km
HAUNG JIAWA SHAN Offset of Qc Channel Beds 5.8-7.6 km Offset of Qta Terrace
...
EOffset of Pre - Silurian Amphibolite 12.9-13.8 km Offset of Western Limit of Pre -
Silurian Marble 14.5-14.8 km Offset of Oligocene Unconformity 14.0-14.1 km
HAUNG JIAWA SHAN Offset of Qc Channel Beds 5.8-7.6 km Offset of Qta Terrace
...
Page 68
Photograph looking northwest at a 10 - m offset of a dry streambed along the
main trace of the Kunlun fault system , the Tuosuohu - Maqu - Xidatan fault , near
35.75 ° N , 95.15 ° E ( See Kidd & Molnar , 1988 ) . Quaternary offsets and rates ...
Photograph looking northwest at a 10 - m offset of a dry streambed along the
main trace of the Kunlun fault system , the Tuosuohu - Maqu - Xidatan fault , near
35.75 ° N , 95.15 ° E ( See Kidd & Molnar , 1988 ) . Quaternary offsets and rates ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Fold shape analysis in the vicinity of North Almora Thrust in District | 121 |
Simla group problem in HimalayaA critical review | 131 |
Geology of Kishanpur NagrotaBasantgarhGujru Nagrota Sector of Inner | 137 |
8 other sections not shown
Other editions - View all
Common terms and phrases
active associated average axis beds belt blocks central Chevron Folds compressive stresses crustal deformation developed direction displacement earthquake east east-west eastern estimated et al evidence exposed extension fault field folds Formation formed Garhwal Geol Geology grains granite Group Himalaya Himalayan Geology India indicate Jammu Jour landslide lateral left-lateral limestone lineation Lower major margin measurements melange metamorphism Mineral mm/a Molnar movement Murree normal faulting northern observed occurred oceanic offset ophiolitic orientation phase plane plateau Pradesh present pressure quartz quartzite range References region reported represent result rocks roughly samples sandstones seismic sequence Shan shape shear shortening Simla Sine Waves Siwalik Slates slip solutions southern specimens strain strike-slip faulting structures suggest surface Table Tapponnier tectonic thrust thrust faulting Tibet trending types units Upper valley volcanics western zone