Results 201 to 210 of about 40,548 (279)

Reef building and carbonate production modes in the west-central Tethys during the Cenozoic

Marine and Petroleum Geology, 2017
Luis Pomar, Pamela Hallock, Guillem Mateu-Vicens   +2 more
exaly   +2 more sources

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Petrogenesis of Early Cambrian granitoids in the western Kunlun orogenic belt, Northwest Tibet: Insight into early stage subduction of the Proto-Tethys Ocean

, 2020
The west Kunlun orogenic belt, located on the northwest margin of the Tibetan Plateau, represents a crucial tectonic junction between the central Asia and Tethys domains.
Jiyuan Yin, W. Xiao, Min Sun, Wen Chen, C. Yuan, Yunying Zhang, Tao Wang, Qiuyi Du, Xiangsong Wang, X. Xia   +9 more
semanticscholar   +1 more source

Tectonic Evolution of the Meso-Tethys Ocean: Insights from Geochemistry and Geochronology of the Jurassic ophiolitic complex in the Asa area, central Tibet

Soviet Economy, 2021
Although voluminous Jurassic ophiolites have been reported along the Bangong–Nujiang Suture Zone (BNSZ), the tectonic setting of ophiolites and the Jurassic evolution history of the Meso-Tethys Ocean remain mysterious.
Xiao-wen Zeng, Ming Wang, Yunpeng Yu, Hang Li, Xianjin Zeng, Di Shen   +5 more
semanticscholar   +1 more source

Paleomagnetism of Middle Triassic Lavas From Northern Qiangtang (Tibet): Constraints on the Closure of the Paleo‐Tethys Ocean

Journal of Geophysical Research: Solid Earth, 2020
We present results from a paleomagnetic study of Middle Triassic lavas (~242–240 Ma) from the northern Qiangtang block to improve our understanding of the timing and kinematics of the closure of the eastern Paleo‐Tethys Ocean.
Peiping Song, L. Ding, P. Lippert, Zhenyu Li, Liyun Zhang, Jing Xie   +5 more
semanticscholar   +1 more source

Syn-depositional continental rifting of the Southeastern Neo-Tethys margin during the Albian–Cenomanian: evidence from stratigraphic correlation

Soviet Economy, 2020
Albian–Cenomanian successions (Kazhdumi and Sarvak formations) represent remarkable variations in thickness, facies, fauna, and environments throughout the Zagros area.
A. Navidtalab, M. Sarfi, A. Enayati-Bidgoli, Mohsen Yazdi-Moghadam   +3 more
semanticscholar   +1 more source

Triassic Sedimentary Filling and Closure of the Eastern Paleo‐Tethys Ocean: New Insights From Detrital Zircon Geochronology of Songpan‐Ganzi, Yidun, and West Qinling Flysch in Eastern Tibet

Tectonics, 2019
Triassic flysch in the Songpan‐Ganzi Complex (SGC), eastern Tibet, is an important and rich record of tectonism associated with evolution and closure of the eastern Paleo‐Tethys Ocean.
X. Jian, A. Weislogel, A. Pullen
semanticscholar   +1 more source

Synchronized changes in shallow water carbonate production during the Carnian Pluvial Episode (Late Triassic) throughout Tethys

, 2020
Quantitative petrologic analysis on carbonates was carried out on stratigraphic sections encompassing the Carnian Pluvial Episode from northwestern Sichuan Basin, South China and eastern Southern Alps.
Xin Jin, P. Gianolla, Zhiqiang Shi, M. Franceschi, M. Caggiati, Yixing Du, N. Preto   +6 more
semanticscholar   +1 more source

Early Neogene foreland of the Zagros, implications for the initial closure of the Neo-Tethys and kinematics of crustal shortening

Earth and Planetary Science Letters, 2017
Mortaza Pirouz, Jean Philippe Avouac, Jamshid Hassanzadeh   +2 more
exaly   +2 more sources

The Cretaceous Tethys

1995
Cretaceous transgressions left marine deposits over wide areas of Tethys, from which it is possible to develop paleogeographic maps depicting the configuration and extent of marine and continental paleoenvironments, including oceanic seafloor and structural patterns.
Jean-Pierre Masse, Jean Philip, Gilbert Camoin   +2 more
openaire   +1 more source

Mediterranean and Tethys

1977
The boundary between the Eurasian and the African plates, formerly the suture between Eurasia and Gondwana, has been the locus of violent tectonic diastrophism and rapidly changing geography since the Triassic. The Mesozoic seas, and sometimes the Paleozoic seas, of this zone and its extension into the Himalayan region are known as the Tethys (Neumayr,
Hans Laubscher, Daniel Bernoulli
openaire   +1 more source