Zobrazeno 1 - 10
of 46
pro vyhledávání: '"Schenker, F.L."'
Publikováno v:
In Tectonophysics 5 December 2012 579:88-103
Autor:
Corvò S.[1, Maino M.[1, Langone A.[2], Schenker F.L.[3], Piazolo S.[4], Casini L.[5], Seno S.[1
Publikováno v:
Lithos (Oslo. Print) 390-391 (2021): 1–25. doi:10.1016/j.lithos.2021.106126
info:cnr-pdr/source/autori:Corvò S.[1,2], Maino M.[1,2], Langone A.[2], Schenker F.L.[3], Piazolo S.[4], Casini L.[5], Seno S.[1,3]/titolo:Local variations of metamorphic record from compositionally heterogeneous rocks (Cima di Gagnone, Central Alps): Inferences on exhumation processes of (U)HP-HT rocks/doi:10.1016%2Fj.lithos.2021.106126/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:390-391
info:cnr-pdr/source/autori:Corvò S.[1,2], Maino M.[1,2], Langone A.[2], Schenker F.L.[3], Piazolo S.[4], Casini L.[5], Seno S.[1,3]/titolo:Local variations of metamorphic record from compositionally heterogeneous rocks (Cima di Gagnone, Central Alps): Inferences on exhumation processes of (U)HP-HT rocks/doi:10.1016%2Fj.lithos.2021.106126/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:390-391
The record of metamorphic conditions is commonly highly heterogeneous in spatially close rocks of different composition and rheology. The well-studied Cima di Gagnone area in the Central Alps represents such an example, as relatively small, 1– to 1
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f8bce488539f23e5f25361240b26d11
http://www.cnr.it/prodotto/i/455988
http://www.cnr.it/prodotto/i/455988
Akademický článek
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Raman elastic geobarometry has increasingly been used complementary to metamorphic phase equilibria to estimate the conditions of recrystallization in metamorphic rocks. The procedure of applying Raman elastic barometry to host-inclusion mineral syst
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::f75f6995861284cc35521358a11917b0
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3068576
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3068576
Carbonatitic dykes surrounded by K-Na-fenites were discovered in the Pelagonian Zone in Greece. Their carbonate portions have an isotopic mantle signature of δ13C and δ18O ranging from −5.18 to −5.56 (‰ vs. VPDB) and from 10.68 to 11.59 (‰
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::a78eb50375c3fcc121eed0f99df9abec
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069261
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069261
The synmetamorphic nappe system of the Rhodope Metamorphic Complex has been deformed into dome-and-basin structures attributed to syn- to post-convergent exhumation. We document the deformation style and present new thermobarometric and geochronologi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::5a1529bbc3d6cb1cbcbc355a395b5a31
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069368
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3069368
Akademický článek
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The magmatic history of the Pelagonian Zone, in northern Greece, is constrained with secondary ion mass spectrometer (SIMS) U-Pb dating on zircons of various granitoids whose structural positions were defined with respect to the regional main foliati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2127::3f0139f1c240f6b63eebbdd7605d2902
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3070008
https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3070008
Akademický článek
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