About: High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint

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About: High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint Goto Sponge NotDistinct Permalink

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article by Shah Wali Faryad & Jiří Žák published March 2016 in Lithos

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rdf:type	Item
description	wetenschappelijk artikel (nl) наукова стаття, опублікована в березні 2016 (uk) im März 2016 veröffentlichter wissenschaftlicher Artikel (de) article by Shah Wali Faryad & Jiří Žák published March 2016 in Lithos (en)
publication date	wds:Q57571714-6BDAED20-72FD-4E3A-9213-C321B0AFD5D3
publication date	2016-03-01 00:00:00Z (xsd:dateTime)
rdfs:label	High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint (en) High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint (nl)
skos:prefLabel	High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint (en) High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint (nl)
name	High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint (en) High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint (nl)
author	wds:Q57571714-05D00EDC-7145-4A44-9102-8F38962F010A wds:Q57571714-0AF043B2-EED9-4B53-8602-DE295453E413
author	Jiří Žák Shah Wali Faryad
title	wds:Q57571714-5AF4A156-011E-45D4-A109-D1AA012EF01C
title	High-pressure granulites of the Podolsko complex, Bohemian Massif: An example of crustal rocks that were subducted to mantle depths and survived a pervasive mid-crustal high-temperature overprint (en)
page(s)	wds:Q57571714-5A0DF39D-8D9B-45C7-BD47-63A4348B7B8F
page(s)	246-260
instance of	wds:Q57571714-13026E18-E9E6-4F23-B64F-E693B5C50BF8
instance of	scholarly article
published in	wds:Q57571714-13E72EE8-A126-451A-9CE2-6EAEE70AAA34
published in	Lithos
volume	wds:Q57571714-FA08AA5C-3015-4CE5-AA62-191F3F2ED3D1
volume	246-247
DOI	wds:Q57571714-120F68E2-7B3A-4F22-8E5E-10945325E874
DOI	http://dx.doi.org/10.1016/J.LITHOS.2016.01.005
DOI	10.1016/J.LITHOS.2016.01.005
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q57571714
is cites work of	How far did the Cadomian ʽterranesʼ travel from Gondwana during early Palaeozoic? A critical reappraisal based on detrital zircon geochronology Rapid extensional unroofing of a granite–migmatite dome with relics of high-pressure rocks, the Podolsko complex, Bohemian Massif European Variscan orogenic evolution as an analogue of Tibetan-Himalayan orogen: Insights from petrology and numerical modeling
is cites work of	wds:Q57571691-FC5A4855-BF4A-4825-AF05-C243CE7389B0 wds:Q57571705-3F0A23FD-1F46-4859-B5CB-1C125C40FE30 wds:Q57861314-C27117E6-2B8D-4211-BBAA-CC99168177EF

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