FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006879244> ?p ?o ?g. }

• W2006879244 endingPage "603" @default.
• W2006879244 startingPage "587" @default.
• W2006879244 abstract "Abstract Two impure ultrahigh‐pressure (UHP) marbles, a calcite marble with the peak assemblage Grt + Phe + Cpx + Rt + (Arg) and a dolomite marble with the peak assemblage Crn + Chl + Rt + Dol (±Arg), from the same lens from the polymetamorphic complex of the Brossasco‐Isasca Unit (BIU) (southern Dora‐Maira Massif) have been petrologically investigated and modelled by calculating P – T phase‐diagram projections for H 2 O–CO 2 mixed‐volatile systems. Thermobarometric data obtained from the calcite marble suggest Alpine peak conditions in the diamond stability field (4.0 GPa at 730 °C), and allow reconstruction of the earlier portion of the Alpine retrograde P – T path, which is characterized by a significant decompression coupled with a moderate and continuous cooling to 650 °C at 2.50 GPa. The modelled fluid compositions at peak conditions point to 0.025 ≤ X (CO 2 ) ≤ 0.10 and X (CO 2 ) ≤ 0.0012 in the calcite marble and dolomite marble, respectively, suggesting fluid heterogeneity at the local scale and an internally buffered fluid evolution of the studied impure marbles. The lack of micro‐diamond in the BIU marbles is explained by the very‐low X (CO 2 ) values, which favoured relatively high f O 2 ‐conditions, preventing the formation of diamond at the UHP peak metamorphic conditions." @default.
• W2006879244 created "2016-06-24" @default.
• W2006879244 creator A5022166685 @default.
• W2006879244 creator A5033679938 @default.
• W2006879244 creator A5044713520 @default.
• W2006879244 creator A5082097603 @default.
• W2006879244 date "2007-06-25" @default.
• W2006879244 modified "2023-10-06" @default.
• W2006879244 title "Impure marbles from the UHP Brossasco‐Isasca Unit (Dora‐Maira Massif, western Alps): evidence for Alpine equilibration in the diamond stability field and evaluation of the <i>X</i>(CO₂) fluid evolution" @default.
• W2006879244 cites W1587965322 @default.
• W2006879244 cites W1592718458 @default.
• W2006879244 cites W1767843502 @default.
• W2006879244 cites W1830358639 @default.
• W2006879244 cites W1833791531 @default.
• W2006879244 cites W1973055268 @default.
• W2006879244 cites W1974078246 @default.
• W2006879244 cites W1978514891 @default.
• W2006879244 cites W1978801698 @default.
• W2006879244 cites W1980313149 @default.
• W2006879244 cites W1981238025 @default.
• W2006879244 cites W1981636880 @default.
• W2006879244 cites W1984209897 @default.
• W2006879244 cites W1985297387 @default.
• W2006879244 cites W1993040660 @default.
• W2006879244 cites W1994812683 @default.
• W2006879244 cites W2000995611 @default.
• W2006879244 cites W2003479129 @default.
• W2006879244 cites W2007307178 @default.
• W2006879244 cites W2009436180 @default.
• W2006879244 cites W2022796553 @default.
• W2006879244 cites W2028498366 @default.
• W2006879244 cites W2036931671 @default.
• W2006879244 cites W2045288367 @default.
• W2006879244 cites W2047230097 @default.
• W2006879244 cites W2048696083 @default.
• W2006879244 cites W2054643770 @default.
• W2006879244 cites W2056892579 @default.
• W2006879244 cites W2059099197 @default.
• W2006879244 cites W2069006769 @default.
• W2006879244 cites W2072371392 @default.
• W2006879244 cites W2076628330 @default.
• W2006879244 cites W2091370619 @default.
• W2006879244 cites W2093425736 @default.
• W2006879244 cites W2093701233 @default.
• W2006879244 cites W2103995112 @default.
• W2006879244 cites W2115177642 @default.
• W2006879244 cites W2133075265 @default.
• W2006879244 cites W2138196090 @default.
• W2006879244 cites W2155272764 @default.
• W2006879244 cites W2156270640 @default.
• W2006879244 cites W2159003208 @default.
• W2006879244 cites W2160794451 @default.
• W2006879244 cites W2326602674 @default.
• W2006879244 cites W2343053134 @default.
• W2006879244 cites W2344417902 @default.
• W2006879244 cites W2345944069 @default.
• W2006879244 cites W2361189459 @default.
• W2006879244 cites W2395756718 @default.
• W2006879244 cites W2411551004 @default.
• W2006879244 cites W2435192269 @default.
• W2006879244 cites W2500169225 @default.
• W2006879244 cites W2990672819 @default.
• W2006879244 cites W4300903849 @default.
• W2006879244 cites W2009556281 @default.
• W2006879244 doi "https://doi.org/10.1111/j.1525-1314.2007.00716.x" @default.
• W2006879244 hasPublicationYear "2007" @default.
• W2006879244 type Work @default.
• W2006879244 sameAs 2006879244 @default.
• W2006879244 citedByCount "94" @default.
• W2006879244 countsByYear W20068792442012 @default.
• W2006879244 countsByYear W20068792442013 @default.
• W2006879244 countsByYear W20068792442014 @default.
• W2006879244 countsByYear W20068792442015 @default.
• W2006879244 countsByYear W20068792442016 @default.
• W2006879244 countsByYear W20068792442017 @default.
• W2006879244 countsByYear W20068792442018 @default.
• W2006879244 countsByYear W20068792442019 @default.
• W2006879244 countsByYear W20068792442020 @default.
• W2006879244 countsByYear W20068792442021 @default.
• W2006879244 countsByYear W20068792442022 @default.
• W2006879244 countsByYear W20068792442023 @default.
• W2006879244 crossrefType "journal-article" @default.
• W2006879244 hasAuthorship W2006879244A5022166685 @default.
• W2006879244 hasAuthorship W2006879244A5033679938 @default.
• W2006879244 hasAuthorship W2006879244A5044713520 @default.
• W2006879244 hasAuthorship W2006879244A5082097603 @default.
• W2006879244 hasConcept C127313418 @default.
• W2006879244 hasConcept C160776313 @default.
• W2006879244 hasConcept C17409809 @default.
• W2006879244 hasConcept C191897082 @default.
• W2006879244 hasConcept C192562407 @default.
• W2006879244 hasConcept C199289684 @default.
• W2006879244 hasConcept C26687426 @default.
• W2006879244 hasConcept C2776921476 @default.
• W2006879244 hasConcept C2780181037 @default.
• W2006879244 hasConcept C2780191791 @default.
• W2006879244 hasConceptScore W2006879244C127313418 @default.
• W2006879244 hasConceptScore W2006879244C160776313 @default.

• next