Himalaya: Geological Aspects, Volume 1Contributed articles. |
From inside the book
Results 1-3 of 58
Page 235
THE HAZARA ARC The Hazara arc in northern Pakistan ( Figure 3 ) forms the
northwestern limit of the Indian shield . It is defined by a broad belt of subparallel
structures that delineate an arc convex to the south - southeast . These structures
...
THE HAZARA ARC The Hazara arc in northern Pakistan ( Figure 3 ) forms the
northwestern limit of the Indian shield . It is defined by a broad belt of subparallel
structures that delineate an arc convex to the south - southeast . These structures
...
Page 237
South of the Salt range a number of basement faults are seismically delineated (
Figure 4 ) . The composite fault - plane solutions for these events indicate strike -
slip movement in a right - lateral sense . These solutions agree in orientation ...
South of the Salt range a number of basement faults are seismically delineated (
Figure 4 ) . The composite fault - plane solutions for these events indicate strike -
slip movement in a right - lateral sense . These solutions agree in orientation ...
Page 241
Locations for 62 small earthquakes , obtained from an analysis of two months of
data for the Quetta seismic network ( Figure 8 ) , provide new insight into the
complicated tectonics of the broad region surrounding the Quetta syntaxis .
Locations for 62 small earthquakes , obtained from an analysis of two months of
data for the Quetta seismic network ( Figure 8 ) , provide new insight into the
complicated tectonics of the broad region surrounding the Quetta syntaxis .
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
Tectonics and Structure of the Pamirs | 1 |
Peninsular and Himalayan Precambrian Belts | 31 |
Central Indian Ridge and Himalayan Mountain System | 55 |
Copyright | |
8 other sections not shown
Other editions - View all
Common terms and phrases
active Asia associated base basement basic basin beds belt biotite blocks Boundary Central collision complex consists continental continuous Cretaceous crust crystalline deformation deposits direction early earthquakes east eastern Eocene et al evolution extension facies faults Figure folds followed formation formed Gansser Garhwal Geol Geology gneiss grade granite Group Higher Himalaya Indian Indian plate indicate Indus initial island Jour Kashmir Ladakh Late Lesser levels limestone Lower magmatic major margin metamorphism Middle mountain movement nappe nature Nepal northern observed occur oceanic ophiolite origin orogenic Pakistan palaeomagnetic Palaeozoic Pande phase plate possible Precambrian present Range region represent rocks rotation sampled sandstones schists sedimentary sediments seismicity sequence Shield similar southern structural studies subduction suggested suture Table tectonic Tertiary Tethyan thickness thrust Tibetan trend units Upper valley volcanics western zone