inscription
Portail d'information géographique

Résultats de la recherche (6 résultats)

Affinez votre recherche

Par Collection Par Auteur Par Date Par Sujet Par Titre
  • Neotectonic influences on morphological variations along the coastline of Kachchh, India
  • The coastline of Kachchh in the arid, westernmost part of India can be broadly divided into five major segments. These are, from west to east, the deltaic coast, the irregular drowned prograded coast, the spits and cuspate foreland complex
  • Geomorphic assemblage of the Gulf of Kachchh coast, western India : implications in understanding the pathways of coastal sediments
  • This study is an attempt to examine the textural and compositional characteristics of sediments along the entire coast of Gulf of Kachchh for understanding their pathways and accomadation within different landforms along the Gulf of Kachchh coast
  • Geomorphology of the Little Rann of Kachchh, W.India : implication for basin architecture and Holocene palaeo-oceanographic conditions
  • This study attempts to describe the geomorphic peculiarities of the Little Rann sedimentary basin, a unique terrain located in the southeastern part of the seismically active Kachchh palaeorift graben and represents the uplift floor of a former gulf
  • Tectonic geomorphology and evidence for active tilting of the Bela, Khadir and Bhanjada islands in the seismically active Kachchh palaeorift graben, Western India
  • Erosion littorale ; Faille ; Fossé tectonique ; Gujarāt ; Géomorphologie structurale ; Holocène ; Ile ; Inde ; Kachchh ; Mouvement vertical ; Néotectonique ; Sismicité ; Tectonique
  • The Bela, Khadir and Bhanjada islands form a part of a linear chain of four major islands bound by the E-W trending Island Belt Fault (IBF) in the northern part of the seismically active Kachchh palaeorift basin. The islands are discrete tilt blocks
  • Active tectonic control on alluvial fan architecture along Kachchh mainland Hill Range, Western India
  • view, a shallow sea linked the Gulf of Kachchh to the Gulf of Khambhat only in a time period around Marine Isotope Stage 5. The studies also suggest that the Nal region itself may not have witnessed any major uplift (beyond 10 m) during late Quaternary.