FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3012024664> ?p ?o ?g. }

• W3012024664 endingPage "6324" @default.
• W3012024664 startingPage "6296" @default.
• W3012024664 abstract "A set of granite porphyry (grnt‐porphyry) and sub‐rhyolite porphyry (rhy‐porphyry) with specific blue quartz phenocrysts was disintegrated in the northern Kongling terrane, China. Geochemical and isotopic analyses were performed on samples from Kongziqiao (KZQ) and Baizhuping (BZP). In terms of major elements, both are rich in silicon and alkalis, but depleted in calcium and magnesium. Their trace element contents are also similar, exhibiting negative anomalies for large‐ion lithophile elements (LILEs) such as K, Rb and Sr but positive anomalies for high‐field‐strength elements (HFSEs) such as Hf, Ce and Lu. Other elements such as Nb, Ti, P, Sm, Ho, Y and Yb show negative anomalies; however, the KZQ grnt‐porphyry is characterized by positive Ba and negative Zr anomalies; whereas the BZP sub rhy‐porphyry has negative Ba, U and Ta anomalies. The overall geochemistry is characteristic of A‐type granite formed in an extensional environment (A 2 ‐type). Yield ages of the KZQ grnt‐porphyry are (2,239 Ma) and that of the BZP (1,895 Ma) sub rhy‐porphyry are Paleoproterozoic. Analysis of Hf isotopes shows that both have negative ε Hf (t) values, but the ε Hf (t) value of the KZQ grnt‐porphyry is slightly more positive (minimum −12.4; mean − 8.8) and its depleted mantle model age (T DM1 = 2.85–3.06 Ga, mean 2.92 Ga) is slightly older than the BZP sub rhy‐porphyry (minimum ε Hf (t) = −17.1, mean − 14.9; T DM1 = 2.79–2.92 Ga, mean 2.85 Ga). This suggests that they are derived from partial melting of different generations of ancient crustal material, which implies significant stratification in the Archean crust. The ε Nd (t) values of two samples of each rock type also indicate that both were derived from Ca. 2.9 Ga ancient crust (ε Nd (t) KZQ = −5.58, −4.74; ε Nd (t) BZP = −8.55, −8.22). The petrogenesis of both rock types is related to deep crustal extensional collapse caused by post‐orogenic extension before 2.2 Ga and after 1.9 Ga. The formation of two porphyries represents the changes in tectonic system of the Yangtze Block, and this tectonic evolution may have contributed to the reconstruction of the Columbia supercontinent." @default.
• W3012024664 created "2020-03-23" @default.
• W3012024664 creator A5001639101 @default.
• W3012024664 creator A5004616053 @default.
• W3012024664 creator A5008680864 @default.
• W3012024664 creator A5019178864 @default.
• W3012024664 creator A5031775271 @default.
• W3012024664 creator A5053517777 @default.
• W3012024664 creator A5066737474 @default.
• W3012024664 creator A5076447968 @default.
• W3012024664 creator A5088664989 @default.
• W3012024664 date "2020-03-10" @default.
• W3012024664 modified "2023-10-16" @default.
• W3012024664 title "Two extensional events in the early evolution of the Yangtze Block, South China: Geochemical and isotopic evidence from two sets of Paleoproterozoic alkali porphyry in the Northern Kongling terrane" @default.
• W3012024664 cites W1242895745 @default.
• W3012024664 cites W1475468184 @default.
• W3012024664 cites W1964957427 @default.
• W3012024664 cites W1966039270 @default.
• W3012024664 cites W1969968003 @default.
• W3012024664 cites W1974499954 @default.
• W3012024664 cites W1975676133 @default.
• W3012024664 cites W1977650828 @default.
• W3012024664 cites W1978362794 @default.
• W3012024664 cites W1982272146 @default.
• W3012024664 cites W1988317790 @default.
• W3012024664 cites W1990597841 @default.
• W3012024664 cites W1991381283 @default.
• W3012024664 cites W1992326732 @default.
• W3012024664 cites W1999496681 @default.
• W3012024664 cites W2000555536 @default.
• W3012024664 cites W2002947230 @default.
• W3012024664 cites W2010194005 @default.
• W3012024664 cites W2011613029 @default.
• W3012024664 cites W2013747430 @default.
• W3012024664 cites W2014580760 @default.
• W3012024664 cites W2017722262 @default.
• W3012024664 cites W2019143131 @default.
• W3012024664 cites W2029184354 @default.
• W3012024664 cites W2031423471 @default.
• W3012024664 cites W2033683037 @default.
• W3012024664 cites W2037028362 @default.
• W3012024664 cites W2042803182 @default.
• W3012024664 cites W2042991064 @default.
• W3012024664 cites W2057876276 @default.
• W3012024664 cites W2059250966 @default.
• W3012024664 cites W2065085765 @default.
• W3012024664 cites W2069124235 @default.
• W3012024664 cites W2070718822 @default.
• W3012024664 cites W2074233105 @default.
• W3012024664 cites W2075964210 @default.
• W3012024664 cites W2076143345 @default.
• W3012024664 cites W2076903568 @default.
• W3012024664 cites W2081407886 @default.
• W3012024664 cites W2088223235 @default.
• W3012024664 cites W2089048002 @default.
• W3012024664 cites W2089537292 @default.
• W3012024664 cites W2090587021 @default.
• W3012024664 cites W2093483991 @default.
• W3012024664 cites W2094913826 @default.
• W3012024664 cites W2106963293 @default.
• W3012024664 cites W2108971421 @default.
• W3012024664 cites W2133042542 @default.
• W3012024664 cites W2138522501 @default.
• W3012024664 cites W2140093647 @default.
• W3012024664 cites W2168661179 @default.
• W3012024664 cites W2195516043 @default.
• W3012024664 cites W2296214819 @default.
• W3012024664 cites W2328606495 @default.
• W3012024664 cites W2335208069 @default.
• W3012024664 cites W2441695414 @default.
• W3012024664 cites W2523510373 @default.
• W3012024664 cites W2592142660 @default.
• W3012024664 cites W2617827725 @default.
• W3012024664 cites W2619518091 @default.
• W3012024664 cites W2750989671 @default.
• W3012024664 cites W2769798525 @default.
• W3012024664 cites W2790272406 @default.
• W3012024664 cites W2793593573 @default.
• W3012024664 cites W2801255881 @default.
• W3012024664 cites W2804824192 @default.
• W3012024664 cites W2809607727 @default.
• W3012024664 cites W2888691911 @default.
• W3012024664 cites W2899375247 @default.
• W3012024664 cites W2930553564 @default.
• W3012024664 cites W2979817446 @default.
• W3012024664 cites W4250915572 @default.
• W3012024664 doi "https://doi.org/10.1002/gj.3802" @default.
• W3012024664 hasPublicationYear "2020" @default.
• W3012024664 type Work @default.
• W3012024664 sameAs 3012024664 @default.
• W3012024664 citedByCount "2" @default.
• W3012024664 countsByYear W30120246642021 @default.
• W3012024664 countsByYear W30120246642022 @default.
• W3012024664 crossrefType "journal-article" @default.
• W3012024664 hasAuthorship W3012024664A5001639101 @default.
• W3012024664 hasAuthorship W3012024664A5004616053 @default.
• W3012024664 hasAuthorship W3012024664A5008680864 @default.
• W3012024664 hasAuthorship W3012024664A5019178864 @default.

• next