Results 91 to 100 of about 1,509,261 (248)

Late paleozoic to early mesozoic provenance record of paleo-pacific subduction beneath South China [PDF]

open access: yes, 2015
Northeast trending Yong'an Basin, southeast South China Craton, preserves a Permian-Jurassic, marine to continental, siliciclastic-dominated, retroarc foreland basin succession.
Hu, L.   +4 more
core   +1 more source

Valentin Petrovich Tverdokhlebov (1933–2023) [PDF]

open access: yesИзвестия Саратовского университета. Новая серия: Серия Науки о Земле
Dedication to the memory of a colleague, Doctor of Geological and Mineralogical Sciences Valentin P. Tverdokhlebov, a well-known specialist in sedimentology and palaeogeography of the Late Permian and Triassic of the Eastern Russian Plate and Southern ...
Minikh, Alla Vasilievna   +3 more
doaj   +1 more source

Permian fusulinacean faunas of Thailand — event controlled evolution

open access: yes, 1986
The evolution of the fusulinacean faunas of Thailand during Permian times is controlled by bioevents. The first bioevent happened in the upper Lower Permian and is characterized by the disappearance of the Arctic-Tethyan elements.
Helmcke, Dietrich   +3 more
core   +1 more source

Permian-Triassic brachiopod fauna and the end-Permian mass extinction

open access: yes, 2014
Permian-Triassic brachiopod fauna and the end-Permian mass ...
Y Zhang (5998940)
core  

Carbon cycle perturbations and environmental change of the middle permian and Late Triassic Paleo-Antarctic circle

open access: yesScientific Reports
During the middle Permian through the Triassic, Tasmania moved from paleo-latitudes of 78° to 69°S, wedged between Antarctica and Australia, within the paleo-South polar circle.
Wahyuningrum Lestari   +4 more
doaj   +1 more source

The Upper Permian reefs of South China are last reefs of the Рaleozoic

open access: yesЛитосфера, 2019
Subject of research. The upper Permian reefs of the Yangtze block of southern China are considered. Among them there are two species which differ in location in the basin and the nature of the internal structure.Methods and results.
V. G. Kuznetsov   +2 more
doaj   +1 more source

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