Results 161 to 170 of about 1,836 (211)
Evidence of low velocity layers at the top and bottom of the Mantle Transition Zone (MTZ) below the Uttarakhand Himalaya, India. [PDF]
Sci RepMandal P, Saha S, Prathigadapa R.
europepmc +1 more source
Provenance of late Pleistocene loess in central and eastern Europe: isotopic evidence for dominant local sediment sources. [PDF]
Sci RepFenn K +4 more
europepmc +1 more source
A novel approach for studying lithospheric deformation driven by asthenospheric flow
Krstekanic N +4 more
europepmc +1 more source
Long-Term Evolution of a Plume-Induced Subduction in the Neotethys Realm
Earth and Planetary Science Letters, 2021 Abstract The head of a mantle plume can weaken the oceanic lithosphere through the combined action of its buoyancy forces and excess temperature, which eventually induces intra-oceanic subductions. However, the dynamics of plume-induced subductions, their lifetime and their ability to propagate at the scale of an entire ocean remain unknown. Here, we
Nicolas Coltice +2 more
exaly +4 more sources
Global and Planetary Change, 2010 End-Permian mass extinction and palaeoenvironmental changes in Neotethys: Evidence from an oceanic carbonate section in southwestern ...
Shu-zhong Shen, Jun Chen, G R Shi
exaly +1 more source
Some of the next articles are maybe not open access.
Related searches:
Related searches:
Journal of the Geological Society, 2023
A complex and chaotic assemblage of the north Croatian inselbergs, considered a geological conundrum, is marked by omnipresent ophiolite mélange. This is a vestige of the unbroken formation of the lithosphere in the northwestern segment of Neotethys during the Mesozoic, spanning from the late Anisian to the late Tithonian.
Damir Slovenec, Branimir Šegvić
openaire +2 more sources
A complex and chaotic assemblage of the north Croatian inselbergs, considered a geological conundrum, is marked by omnipresent ophiolite mélange. This is a vestige of the unbroken formation of the lithosphere in the northwestern segment of Neotethys during the Mesozoic, spanning from the late Anisian to the late Tithonian.
Damir Slovenec, Branimir Šegvić
openaire +2 more sources
Minerals (Basel, Switzerland), 2023 In the Cenomanian, the southern passive margin of the Neotethys Ocean was dominated by a giant carbonate factory. This succession is known as Sarvak Formation, a significant reservoir in Iran. This study focuses on a detailed analysis of facies variations and paleoenvironmental reconstruction, including the interpretation of the platform types, during ...
Vahid Tavakoli
exaly +2 more sources
The early history of the Neotethys archived in the ophiolitic mélange of northwestern Croatia
Journal of the Geological Society, 2023Ophiolite exposures in NW Croatia have been attributed to the Western Vardar Ophiolitic Unit and interpreted as derived from the Meliata–Maliac–Vardar branch of the Neotethys Ocean. Blocks within the ophiolitic mélange on Mt Ivanščica were investigated to determine the petrological and geochemical characteristics of the effusive rocks and ...
Duje Kukoč +7 more
openaire +2 more sources
Journal of Asian Earth Sciences, 2006 We report on an integrated study of a critical segment of the Tauride thrust belt in SE Turkey (Berit area). Units related to two sutures are exposed in the northerly and southerly parts of the area studied.
Timur Ustaömer +2 more
exaly +2 more sources
Neotethys Seawater Chemistry and Temperature at the Dawn of the End Permian Mass Extinction
Gondwana Research, 2016 Abstract The end of the Permian was a time of great death and massive upheaval in the biosphere, atmosphere and hydrosphere. Over the last decades, many causes have been suggested to be responsible for that catastrophe such as global warming, anoxia and acidification.
Karem Azmy +2 more
exaly +4 more sources