Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Alexei L. Perchuk"'
Publikováno v:
Gondwana Research. 119:186-203
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32ca8ce4bed5efe741eb7361fe7a4dc5
https://doi.org/10.1016/j.gr.2023.03.015
https://doi.org/10.1016/j.gr.2023.03.015
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-12 (2021)
Scientific Reports
Scientific Reports
Partial melting of mantle peridotites at spreading ridges is a continuous global process that forms the oceanic crust and refractory, positively buoyant residues (melt-depleted mantle peridotites). In the modern Earth, these rocks enter subduction zo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a76dc3ddc7a47dfd12375e1449e5beb4
https://doaj.org/article/a042816e5bdc40dfb20898a07e572ccd
https://doaj.org/article/a042816e5bdc40dfb20898a07e572ccd
Publikováno v:
Nature. 586:395-401
The ancient cores of continents (cratons) are underlain by mantle keels-volumes of melt-depleted, mechanically resistant, buoyant and diamondiferous mantle up to 350 kilometres thick, which have remained isolated from the hotter and denser convecting
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a01d553e0f723b4d82dfa51f34a8e4b7
https://doi.org/10.1038/s41586-020-2806-7
https://doi.org/10.1038/s41586-020-2806-7
Publikováno v:
Russian Geology and Geophysics. 61:571-591
—The phase relations and melting of subducting sediment were studied in two series of high-pressure experiments at 750– 900 °C and 2.9 GPa and by thermodynamic modeling. In the runs we used a chemical mixture corresponding in composition to glob
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d7eb21f6fe4c6c8f97f860406ce6fe19
https://doi.org/10.15372/rgg2019177
https://doi.org/10.15372/rgg2019177
Publikováno v:
Moscow University Geology Bulletin. 75:254-267
The results of U–Pb zircon dating, as well as the petrologic-geochemical study of samples of zircon-bearing garnet–biotite plagiogneiss and quartz—plagioclase–amphibole granofels from the Vishnevogorsky sequence of the oldest rocks of the Eas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8db736cd350110c59454529f3d13e21
https://doi.org/10.3103/s0145875220030072
https://doi.org/10.3103/s0145875220030072
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :51-62
In the article present results of U-Pb — dating of zircons and petrologic-geochemical study of garnet-biotite plagiogneises and quartz-plagioclase-amphibole granofels host rocks samples from Vishnevogorsky sequence of the oldest rocks of the southe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5591a70702fc95756dc4a53e71032429
https://doi.org/10.33623/0579-9406-2020-2-51-62
https://doi.org/10.33623/0579-9406-2020-2-51-62
Publikováno v:
Petrology. 27:467-488
We present the results of analogue experiments carried out in a piston–cylinder apparatus at 750–900°C and 2.9 GPa aimed to simulate metasomatic transformation of the fertile mantle caused by fluids and melts released from the subducting sedimen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b323d5007eac2a7dc8683b954055c4f
https://doi.org/10.1134/s0869591119050035
https://doi.org/10.1134/s0869591119050035
Publikováno v:
Precambrian Research. 330:20-34
On contemporary Earth, subduction recycles mafic oceanic crust and associated volatile elements, creating new silicic continental crust in volcanic arcs. However, if the mantle was hotter in the Precambrian, the style of subduction, the depth of devo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df682461002622327109395b11ef166a
https://doi.org/10.1016/j.precamres.2019.04.023
https://doi.org/10.1016/j.precamres.2019.04.023
Publikováno v:
Moscow University Geology Bulletin. 74:321-331
This work presents the results of a detailed petrological study of olivine gabbro transformed to a different extent during the eclogite facies metamorphism. The textural features of cumulate crystallization in the rock at the magmatic stage are prese
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e156691b3dd19afa515b7c3d829871ad
https://doi.org/10.3103/s0145875219030050
https://doi.org/10.3103/s0145875219030050
Publikováno v:
Petrology. 27:124-145
The Marun-Keu Complex of high-pressure rocks comprises granitoids, gneisses schists, gabbroids, and peridotites, which are unevenly and variably metamorphosed to the eclogite facies. A representative sample of garnet–amphibole lherzolite from the M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b07d8501c544c974c8700af0272d056
https://doi.org/10.1134/s0869591119020061
https://doi.org/10.1134/s0869591119020061