FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2600163603> ?p ?o ?g. }

• W2600163603 endingPage "148" @default.
• W2600163603 startingPage "130" @default.
• W2600163603 abstract "Garnet in high-pressure (HP) to ultrahigh-pressure (UHP) metamorphic rocks in subduction zone commonly shows considerable zonation in major and trace elements as well as mineral inclusions, which bears information on its growth mechanism via metamorphic or peritectic reactions in coexistence with relic minerals and metamorphic fluids or anatectic melts at subduction-zone conditions. It provides an important target to retrieve physicochemical changes in subduction-zone processes, including those not only in pressure and temperature but also in the durations of metamorphism and anatexis. Garnet from different compositions of HP to UHP metamorphic rocks may show different types of major and trace element zonation, as well as mineral inclusions. Discrimination between the different origins of garnet provides important constraints on pressure and temperature and the evolution history for the HP to UHP metamorphic rocks. Magmatic garnet may occur as relics in granitic gneisses despite metamorphic modification at subduction-zone conditions, with spessartine-increasing or flat major element profiles from inner to outer core and exceptionally higher contents of trace elements than metamorphic mantle and rim. Metamorphic garnet can grow at different metamorphic stages during prograde subduction and retrograde exhumation, with spessartine-decreasing from core to rim if the intracrystalline diffusion is not too fast. The compositional profiles of metamorphic garnet in the abundances of grossular, almandine and pyrope are variable depending on the composition of host rocks and co-existing minerals. Peritectic garnet grows through peritectic reactions during partial melting of HP to UHP rocks, with the composition of major elements to be controlled by anatectic P-T conditions and the compositions of parental rocks and anatectic melts. Trace element profiles in garnet with different origins are also variable depending on the coexisting mineral assemblages, the garnet-forming reactions and the property of metamorphic fluids or anatectic melts. Mineral inclusions not only present key clues to identify the different origins of garnet, but also serve as sound candidates for the temporal constraint on garnet growth." @default.
• W2600163603 created "2017-04-07" @default.
• W2600163603 creator A5002795605 @default.
• W2600163603 creator A5080373149 @default.
• W2600163603 date "2017-09-01" @default.
• W2600163603 modified "2023-10-15" @default.
• W2600163603 title "Different origins of garnet in high pressure to ultrahigh pressure metamorphic rocks" @default.
• W2600163603 cites W1494415438 @default.
• W2600163603 cites W1497952855 @default.
• W2600163603 cites W1523733318 @default.
• W2600163603 cites W1536496118 @default.
• W2600163603 cites W1553008048 @default.
• W2600163603 cites W1570426563 @default.
• W2600163603 cites W1587965322 @default.
• W2600163603 cites W1595459318 @default.
• W2600163603 cites W1856019848 @default.
• W2600163603 cites W1898464489 @default.
• W2600163603 cites W1907449780 @default.
• W2600163603 cites W1944113931 @default.
• W2600163603 cites W1949793175 @default.
• W2600163603 cites W1965656370 @default.
• W2600163603 cites W1965672065 @default.
• W2600163603 cites W1966707406 @default.
• W2600163603 cites W1968228897 @default.
• W2600163603 cites W1970270960 @default.
• W2600163603 cites W1972112327 @default.
• W2600163603 cites W1972614550 @default.
• W2600163603 cites W1973844707 @default.
• W2600163603 cites W1974240514 @default.
• W2600163603 cites W1975652198 @default.
• W2600163603 cites W1978534444 @default.
• W2600163603 cites W1978958059 @default.
• W2600163603 cites W1981713868 @default.
• W2600163603 cites W1981741514 @default.
• W2600163603 cites W1981985528 @default.
• W2600163603 cites W1983298378 @default.
• W2600163603 cites W1984351481 @default.
• W2600163603 cites W1985048272 @default.
• W2600163603 cites W1985297387 @default.
• W2600163603 cites W1985391069 @default.
• W2600163603 cites W1987599461 @default.
• W2600163603 cites W1989192163 @default.
• W2600163603 cites W1990381508 @default.
• W2600163603 cites W1992211265 @default.
• W2600163603 cites W1993307882 @default.
• W2600163603 cites W1994292806 @default.
• W2600163603 cites W1997416903 @default.
• W2600163603 cites W1998611435 @default.
• W2600163603 cites W2000735125 @default.
• W2600163603 cites W2001018270 @default.
• W2600163603 cites W2003809053 @default.
• W2600163603 cites W2005022719 @default.
• W2600163603 cites W2005857471 @default.
• W2600163603 cites W2007170137 @default.
• W2600163603 cites W2008793222 @default.
• W2600163603 cites W2012542327 @default.
• W2600163603 cites W2012657579 @default.
• W2600163603 cites W2013290330 @default.
• W2600163603 cites W2013579065 @default.
• W2600163603 cites W2014884757 @default.
• W2600163603 cites W2015222366 @default.
• W2600163603 cites W2015271179 @default.
• W2600163603 cites W2017649324 @default.
• W2600163603 cites W2020139762 @default.
• W2600163603 cites W2022628471 @default.
• W2600163603 cites W2026783686 @default.
• W2600163603 cites W2027975305 @default.
• W2600163603 cites W2028327545 @default.
• W2600163603 cites W2028330480 @default.
• W2600163603 cites W2029243975 @default.
• W2600163603 cites W2029602159 @default.
• W2600163603 cites W2037313368 @default.
• W2600163603 cites W2038124104 @default.
• W2600163603 cites W2038727385 @default.
• W2600163603 cites W2038984337 @default.
• W2600163603 cites W2039322203 @default.
• W2600163603 cites W2040903195 @default.
• W2600163603 cites W2042627304 @default.
• W2600163603 cites W2042816588 @default.
• W2600163603 cites W2043657636 @default.
• W2600163603 cites W2045171075 @default.
• W2600163603 cites W2045486459 @default.
• W2600163603 cites W2046694869 @default.
• W2600163603 cites W2047486595 @default.
• W2600163603 cites W2049104087 @default.
• W2600163603 cites W2049606755 @default.
• W2600163603 cites W2049916960 @default.
• W2600163603 cites W2051402121 @default.
• W2600163603 cites W2052045614 @default.
• W2600163603 cites W2053040249 @default.
• W2600163603 cites W2053671140 @default.
• W2600163603 cites W2054312647 @default.
• W2600163603 cites W2057322726 @default.
• W2600163603 cites W2058534321 @default.
• W2600163603 cites W2059513771 @default.
• W2600163603 cites W2059947094 @default.
• W2600163603 cites W2062578168 @default.
• W2600163603 cites W2066806818 @default.

• next