Results 1 to 10 of about 1,105,251 (141)
India‐Asia convergence: Insights from burial and exhumation of the Xigaze fore‐arc basin, south Tibet [PDF]
Journal of Geophysical Research: Solid Earth, 2017 AbstractThe composite fore‐arc/syncollisional Xigaze basin in south Tibet preserves a key record of India‐Asia collision. New apatite fission track and zircon (U‐Th)/He data from an N‐S transect across the preserved fore‐arc basin sequence near Xigaze show a consistent northward Late Cretaceous to middle Miocene younging trend, while coexisting apatite
Barry Köhn, Zhiqin Xu, Guangwei Li
exaly +5 more sources
Metamorphic and Thermal History of a Fore-Arc Basin: the Fossil Bluff Group, Alexander Island, Antarctica [PDF]
Journal of Petrology, 2004 The Himalia Ridge Formation (Fossil Bluff Group), Alexander Island is a 2.2-km-thick sequence of Upper Jurassic-Lower Cretaceous conglomerates, sandstones and mudstones, derived from an andesitic volcanic arc and deposited in a fore-arc basin. The metamorphic and thermal history of the formation has been determined using authigenic mineral assemblages ...
Miller, S., MacDonald, D.I.M.
exaly +5 more sources
Long‐term fore‐arc basin evolution in response to changing subduction styles in southern Alaska [PDF]
Tectonics, 2016 AbstractDetrital zircon U‐Pb and fission track double‐dating and Hf isotopes from the Mesozoic and Cenozoic strata in the southern Alaska fore‐arc basin system reveal the effects of two different modes of flat‐slab subduction on the evolution of the overriding plate.
Sarah Falkowski +2 more
exaly +2 more sources
Palaeogeography, Palaeoclimatology, Palaeoecology, 1999 The Cenozoic Quillagua-Llamara basin (northern Chile, Central Andes) is an asymmetrical, intramassif fore-arc basin with a relatively wide northern sector separated from a narrower southward extension by a basement threshold. The north- ern sector was characterised by a noticeable Oligocene?-late Neogene alluvial-fan and lacustrine dominated deposition
Alberto Sáez, G Chong
exaly +3 more sources
Tectono-sedimentary evolution of the NE Dinarides margin during the Cretaceous Adria-Europe convergence [PDF]
Geološki Anali Balkanskoga Poluostrva, 2023 The Cretaceous sedimentation along the NE Dinarides margin occurred in basins above the Europe-dipping Neotethyan Sava subduction zone positioned between Adria- and Europe-derived continental units.
Stojadinović Uroš, Krstekanić Nemanja
doaj +1 more source
Evolution and geodynamic background of Myanmar petroliferous basin group
地质科技通报, 2021 Based on the analysis of the geological records of different tectonic units, and combined with plate reconstruction and geodynamic background, the evolution and their geodynamic background of Myanmar petroliferous basin group are discussed in this paper ...
Ying Wang, Renchen Xin
doaj +1 more source
Geosystems and Geoenvironment, 2023 The Kabaw Fault is a north-south trending arcuate suture zone formed between the accretionary prism of the Indo-Myanmar Ranges (IMR), and the Central Myanmar Basin (CMB). The lineament of the Kabaw Fault is defined as a stratigraphic contact zone between
Kyi Khin +3 more
doaj +1 more source
Evolution of a Fore-Arc Basin, Luzon, Philippines: ABSTRACT [PDF]
AAPG Bulletin, 1982 The Tertiary Central Valley of Luzon is a remarkably well-exposed fore-arc basin, with both the trenchward and arc flanks uplifted and dissected. A study of outcrop geology, drilling results, and seismic reflection records determined the changing geometry of the basin through time, facies distributions, sediment-distribution patterns, and hydrocarbon ...
Steven B. Bachman +2 more
openaire +1 more source
Petroleum Exploration and Development, 2021 Classification, superimposed evolution and sedimentary filling of prototype basins are analyzed based on the Wilson cycle principle of plate theory, by dissecting the evolution history of 483 sedimentary basins around the world since the Precambrian ...
Lirong DOU, Zhixin WEN
doaj +1 more source
Understanding fossil fore-arc basins: Inferences from the Cretaceous Adria-Europe convergence in the NE Dinarides [PDF]
Global and Planetary Change, 2018 The evolution of relict fore-arc basins and their kinematic relationships with sedimentation is often less well understood due their fragmentation or amalgamation of individual basins and continental units by the subsequent collision or other post-orogenic deformation.
Toljić, Marinko +4 more
openaire +2 more sources