Journal of Himalayan Geology, Volume 3Wadia Institute of Himalayan Geology, 1992 - Geology |
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Page 68
( 1982 ) mapped a sequence of moraines , fluvial gravel and lake deposits just
south of the Xidatan - TuosuohuMaqu fault , and within the oldest moraine they
found blocks of pyroxenite with no obvious local source ( Fig . 22 ) . The only
outcrop ...
( 1982 ) mapped a sequence of moraines , fluvial gravel and lake deposits just
south of the Xidatan - TuosuohuMaqu fault , and within the oldest moraine they
found blocks of pyroxenite with no obvious local source ( Fig . 22 ) . The only
outcrop ...
Page 69
Overlying the Triassic formations , is a sequence of ground moraine , fluvial
gravel , varved lake sediment , and another moraine . Both moraines contain
clasts of Triassic rock and granite , and the lower moraine also contains gabbro
and ...
Overlying the Triassic formations , is a sequence of ground moraine , fluvial
gravel , varved lake sediment , and another moraine . Both moraines contain
clasts of Triassic rock and granite , and the lower moraine also contains gabbro
and ...
Page 80
... surroundings of the landslide , the thickness of silty - sandy regolith varies from
1 to 5 m . In the zone of gentle colluvial fan , the loose deposits reach 30 m or so ,
and include gravel and stony layers as well as siltyclay impermeable horizons .
... surroundings of the landslide , the thickness of silty - sandy regolith varies from
1 to 5 m . In the zone of gentle colluvial fan , the loose deposits reach 30 m or so ,
and include gravel and stony layers as well as siltyclay impermeable horizons .
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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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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