Matches in SemOpenAlex for { <https://semopenalex.org/work/W1992214963> ?p ?o ?g. }
- W1992214963 endingPage "1552" @default.
- W1992214963 startingPage "1503" @default.
- W1992214963 abstract "Western Shangdong Province experienced major crustal growth as a result of 2.75 to 2.50 Ga tectonothermal events, different from other Archean areas in the North China Craton. Besides early Neoarchean tonalite-trondhjemite-granodiorite (TTG) and supracrustal assemblages, there are large volumes of late Neoarchean gabbroic, dioritic and granitic rocks in western Shandong. SHRIMP zircon dating of thirty-one samples of different rock types from late Neoarchean rocks yielded a narrow age range from 2560 to 2490 Ma. Based on these data and previously published results, the following conclusions can be drawn: 1) the Archean basement can be divided into three belts: a Late Neoarchean (2525-2490 Ma) crustally-derived granite belt in the northeast, an Early Neoarchean (2.75-2.60 Ga) rock belt in the center, and a Late Neoarchean (2550-2500 Ma) belt of juvenile rocks in the southwest; 2) the tectonic regime in western Shandong Province probably changed from compressional to extensional at around 2525 Ma (between 2530 and 2520 Ma); 3) crustal recycling with addition from the mantle occurred at the end of the Neoarchean; 4) the late Archean magmatic rocks were probably formed in an arc environment." @default.
- W1992214963 created "2016-06-24" @default.
- W1992214963 creator A5002277002 @default.
- W1992214963 creator A5003311999 @default.
- W1992214963 creator A5043922121 @default.
- W1992214963 creator A5047762839 @default.
- W1992214963 creator A5059885564 @default.
- W1992214963 creator A5061270235 @default.
- W1992214963 creator A5061446409 @default.
- W1992214963 creator A5063090553 @default.
- W1992214963 creator A5068497750 @default.
- W1992214963 creator A5069365665 @default.
- W1992214963 creator A5078055442 @default.
- W1992214963 creator A5079202638 @default.
- W1992214963 date "2010-12-01" @default.
- W1992214963 modified "2023-10-14" @default.
- W1992214963 title "Juvenile magmatism and crustal recycling at the end of the Neoarchean in Western Shandong Province, North China Craton: Evidence from SHRIMP zircon dating" @default.
- W1992214963 cites W1965877271 @default.
- W1992214963 cites W1969341864 @default.
- W1992214963 cites W1977431633 @default.
- W1992214963 cites W1977930002 @default.
- W1992214963 cites W1978294483 @default.
- W1992214963 cites W1982274555 @default.
- W1992214963 cites W1983001059 @default.
- W1992214963 cites W1984191236 @default.
- W1992214963 cites W1986293631 @default.
- W1992214963 cites W1989090951 @default.
- W1992214963 cites W1991730062 @default.
- W1992214963 cites W1992778159 @default.
- W1992214963 cites W1998009521 @default.
- W1992214963 cites W1998765219 @default.
- W1992214963 cites W1999213266 @default.
- W1992214963 cites W2005030647 @default.
- W1992214963 cites W2005851587 @default.
- W1992214963 cites W2008353072 @default.
- W1992214963 cites W2008779539 @default.
- W1992214963 cites W2009127786 @default.
- W1992214963 cites W2013388505 @default.
- W1992214963 cites W2015979936 @default.
- W1992214963 cites W2020553110 @default.
- W1992214963 cites W2027031339 @default.
- W1992214963 cites W2028802548 @default.
- W1992214963 cites W2031239288 @default.
- W1992214963 cites W2033354344 @default.
- W1992214963 cites W2034559901 @default.
- W1992214963 cites W2035970163 @default.
- W1992214963 cites W2036174339 @default.
- W1992214963 cites W2036261610 @default.
- W1992214963 cites W2039145047 @default.
- W1992214963 cites W2042619191 @default.
- W1992214963 cites W2043003723 @default.
- W1992214963 cites W2043218179 @default.
- W1992214963 cites W2047151621 @default.
- W1992214963 cites W2048722334 @default.
- W1992214963 cites W2049406998 @default.
- W1992214963 cites W2057731022 @default.
- W1992214963 cites W2057906067 @default.
- W1992214963 cites W2065162710 @default.
- W1992214963 cites W2068403951 @default.
- W1992214963 cites W2068726160 @default.
- W1992214963 cites W2075740329 @default.
- W1992214963 cites W2077709210 @default.
- W1992214963 cites W2085672146 @default.
- W1992214963 cites W2088105278 @default.
- W1992214963 cites W2131368249 @default.
- W1992214963 cites W2133316685 @default.
- W1992214963 cites W2141075302 @default.
- W1992214963 cites W2145604970 @default.
- W1992214963 cites W2164159475 @default.
- W1992214963 cites W2622131772 @default.
- W1992214963 cites W626101698 @default.
- W1992214963 doi "https://doi.org/10.2475/10.2010.11" @default.
- W1992214963 hasPublicationYear "2010" @default.
- W1992214963 type Work @default.
- W1992214963 sameAs 1992214963 @default.
- W1992214963 citedByCount "135" @default.
- W1992214963 countsByYear W19922149632012 @default.
- W1992214963 countsByYear W19922149632013 @default.
- W1992214963 countsByYear W19922149632014 @default.
- W1992214963 countsByYear W19922149632015 @default.
- W1992214963 countsByYear W19922149632016 @default.
- W1992214963 countsByYear W19922149632017 @default.
- W1992214963 countsByYear W19922149632018 @default.
- W1992214963 countsByYear W19922149632019 @default.
- W1992214963 countsByYear W19922149632020 @default.
- W1992214963 countsByYear W19922149632021 @default.
- W1992214963 countsByYear W19922149632022 @default.
- W1992214963 countsByYear W19922149632023 @default.
- W1992214963 crossrefType "journal-article" @default.
- W1992214963 hasAuthorship W1992214963A5002277002 @default.
- W1992214963 hasAuthorship W1992214963A5003311999 @default.
- W1992214963 hasAuthorship W1992214963A5043922121 @default.
- W1992214963 hasAuthorship W1992214963A5047762839 @default.
- W1992214963 hasAuthorship W1992214963A5059885564 @default.
- W1992214963 hasAuthorship W1992214963A5061270235 @default.
- W1992214963 hasAuthorship W1992214963A5061446409 @default.
- W1992214963 hasAuthorship W1992214963A5063090553 @default.
- W1992214963 hasAuthorship W1992214963A5068497750 @default.