Geomorphology of the Himalaya : a climato-tectonic framework
This paper describes the plate tectonics setting, geology, topography, precipitation, erosion processes, sediment yield, and geomorphology of the Himalaya, and, using a climato-tectonic framework, discusses the north-south variation in geomorphology
This paper presents the results of geophysical, geological and geochemical studies of the eastern Indonesian region and their preliminary interpretations as regards tectonic development in an arc-continent collision zone.
Geomorphic expressions of Quaternary tectonic stress field in the Southern section of the Eastern piedmont fault zone of Taihangshan Mountain.
Distinctive features of the Quaternary tectonic stress field in the study area are indicated by reference to landforms, stratigraphy, faulting, and drainage channels. Interpretation of lineaments on satellite images and valley trends on topographic
Fold tectonics in Gondwana formations of India in Gondwana Five. Selected papers and abstracts of papers.
Gondwana formations occur as outliers on Precambrian rocks along eight prominent river valleys of India. Large-scale fold tectonics are postulated for the coal belts of Mahanadi, Wardha. Godavari, Pench-Kanhar, Ganga (Rajmahal), and Brahmaputra
(Eastern Himalaya), in addition to those earlier postulated for Damodar and Koel-Son Valley fields. It is also demonstrated that major faults, often forming present day boundary faults, were formed by block tectonics during the Tertiary period
Boundary of seismic crustal deformation and its implication in tectonic morphogenesis of Japan in Geography and its boundaries La géographie et ses frontières Geographie und ihre Grenzen.. (In Memory of Hans Boesch)
Alanya batisindaki kiyilarda ilk C 14 tarihlendirmelerinin Isiginda Geç Holosen tektonik hareketleri. (First 14 C datings and Late Holocene tectonic events on the Mediterranean coastline, west of Alanya, southern Turkey)
at about 1550 years B.P. caused an upheaval of these former platforms about 6,5-1,2 m. This event coincides with the seismo-tectonic upheaval of the coastlines of the southern Aegean islands.
According to the regional structural-tectonic and magmatic situation on the territory of the MPR there are three metallogenetic provinces. The mineralizations are essentially bound to the Caledonian, Hercynian and Mesozoic mineralization epochs. (HL).