Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 61
Haiyuan Fault - Liupan Shan Region intersected another segment trending N
160 ° E for 33 km and with right - lateral and reverse components . Vertical offsets
ranged from 2 to 6 m and reached a maximum near the intersection with the first ...
Haiyuan Fault - Liupan Shan Region intersected another segment trending N
160 ° E for 33 km and with right - lateral and reverse components . Vertical offsets
ranged from 2 to 6 m and reached a maximum near the intersection with the first ...
Page 63
Roughly eastnortheast - west - southwest crustal shortening occurs in the Tianjin
Shan , Mibo Shan , Yanton Shan , and Daluo Shan , where these ranges trend
roughly northnorthwesterly . In the western Tianjing Shan ( Fig . 11 ) , however ...
Roughly eastnortheast - west - southwest crustal shortening occurs in the Tianjin
Shan , Mibo Shan , Yanton Shan , and Daluo Shan , where these ranges trend
roughly northnorthwesterly . In the western Tianjing Shan ( Fig . 11 ) , however ...
Page 66
Yueliang Shan Fig . 16. Satellite image and regional map of the Haiyuan fault ,
the Madong Shan , and the Liupan Shan ( From Burchfiel et al . , 1991 ) . At its
east end , the active trace of the Haiyuan fault diverges southward from its overall
...
Yueliang Shan Fig . 16. Satellite image and regional map of the Haiyuan fault ,
the Madong Shan , and the Liupan Shan ( From Burchfiel et al . , 1991 ) . At its
east end , the active trace of the Haiyuan fault diverges southward from its overall
...
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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 |
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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