FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2560084685> ?p ?o ?g. }

• W2560084685 endingPage "94" @default.
• W2560084685 startingPage "80" @default.
• W2560084685 abstract "In this paper, some potassic and ultrapotassic rocks in the South China Block (SCB) have been recognized, according to a set of new geochronological, geochemical and Sr-Nd isotopic data. Zircon U-Pb dating from six plutons yield consistent crystallization ages of 445–424 Ma. These potassic and ultrapotassic rocks can be geochemically subdivided into three groups. Group 1, represented by the Longchuan gabbro, longmu diabase, Tangshang and Danqian diorite (445–433 Ma), have low silica contents (SiO2 = 47.38–54.16 wt.%), and high MgO (4.21–9.51 wt.%) and total alkalis (Na2O + K2O = 3.08–5.57 wt.%), with K2O/Na2O ratios of 0.62–1.82. They are enriched in LREE and depleted in Ba, Sr and Ta-Nb-Ti, and exhibit relatively high initial 87Sr/86Sr ratios (0.70561–0.71128), low εNd(430 Ma) values (−8.4 to −3.2), suggesting that they were most plausibly generated by the partial metling of enriched mantle source (EMI). Group 2, from the Huwei diorite (424 Ma), have 45.68–52.87 wt.% of SiO2, 5.79–9.25 wt.% of MgO and 52–65 of mg-number. They have significantly higher Th (9.92 ppm), Ce (88.0–115 ppm) concentration and Ce/Yb (27.6–46.8), Th/Yb ratios (2.58–7.99), and relatively low initial 87Sr/86Sr ratios (0.70501–0.70599), and high εNd(430 Ma) values (−2.1 to −1.5). We propose that they originated from the partial melting of the depleted mantle source with subsequent contamination by crustal materials. Group 3, represented by the Daning lamprophyre (∼445 Ma), has SiO2 contents ranging from 41.73 wt.% to 45.22 wt.%, MgO from 13.74 wt.% to 15.16 wt.%, and mg-muber from 73 to 77, with high K2O/Na2O ratios (>2.0). They have 87Sr/86Sr ratios of 0.62912–0.70384 and εNd(t = 430 Ma) values of −6.4 to −6.3, indicating that the source components are close to the EMI source, with significant sediments involved. These Silurian potassic and ultrapotassic rocks in the SCB can be responsible for post-orogenic delamination and intra-plate extension. And the delamination had a small size and a long duration, and a negligible impact." @default.
• W2560084685 created "2016-12-16" @default.
• W2560084685 creator A5013850494 @default.
• W2560084685 creator A5052892649 @default.
• W2560084685 creator A5064119420 @default.
• W2560084685 date "2017-03-01" @default.
• W2560084685 modified "2023-09-27" @default.
• W2560084685 title "Petrogenesis and geodynamic implications of the early Paleozoic potassic and ultrapotassic rocks in the South China Block" @default.
• W2560084685 cites W1533128066 @default.
• W2560084685 cites W1597063492 @default.
• W2560084685 cites W1965270901 @default.
• W2560084685 cites W1965958159 @default.
• W2560084685 cites W1967248360 @default.
• W2560084685 cites W1973191271 @default.
• W2560084685 cites W1973502650 @default.
• W2560084685 cites W1984325281 @default.
• W2560084685 cites W1986337215 @default.
• W2560084685 cites W1987728472 @default.
• W2560084685 cites W1990864352 @default.
• W2560084685 cites W1991575260 @default.
• W2560084685 cites W1998080044 @default.
• W2560084685 cites W2000658638 @default.
• W2560084685 cites W2001772043 @default.
• W2560084685 cites W2002042565 @default.
• W2560084685 cites W2003010591 @default.
• W2560084685 cites W2019034794 @default.
• W2560084685 cites W2019402209 @default.
• W2560084685 cites W2026490691 @default.
• W2560084685 cites W2029349252 @default.
• W2560084685 cites W2030387090 @default.
• W2560084685 cites W2035988625 @default.
• W2560084685 cites W2037052020 @default.
• W2560084685 cites W2038070873 @default.
• W2560084685 cites W2045353711 @default.
• W2560084685 cites W2051640776 @default.
• W2560084685 cites W2059011919 @default.
• W2560084685 cites W2060003735 @default.
• W2560084685 cites W2062720709 @default.
• W2560084685 cites W2069627246 @default.
• W2560084685 cites W2080668882 @default.
• W2560084685 cites W2081184569 @default.
• W2560084685 cites W2081433597 @default.
• W2560084685 cites W2081673195 @default.
• W2560084685 cites W2082513246 @default.
• W2560084685 cites W2083286618 @default.
• W2560084685 cites W2085102081 @default.
• W2560084685 cites W2086820683 @default.
• W2560084685 cites W2087984403 @default.
• W2560084685 cites W2089176789 @default.
• W2560084685 cites W2092044082 @default.
• W2560084685 cites W2095601024 @default.
• W2560084685 cites W2095652195 @default.
• W2560084685 cites W2108425616 @default.
• W2560084685 cites W2111053010 @default.
• W2560084685 cites W2116346512 @default.
• W2560084685 cites W2127664928 @default.
• W2560084685 cites W2129035535 @default.
• W2560084685 cites W2138522501 @default.
• W2560084685 cites W2139066743 @default.
• W2560084685 cites W2144461623 @default.
• W2560084685 cites W2151482982 @default.
• W2560084685 cites W2155838580 @default.
• W2560084685 cites W2164723659 @default.
• W2560084685 cites W2166978438 @default.
• W2560084685 cites W2486040615 @default.
• W2560084685 cites W4245638129 @default.
• W2560084685 doi "https://doi.org/10.1016/j.jseaes.2016.12.013" @default.
• W2560084685 hasPublicationYear "2017" @default.
• W2560084685 type Work @default.
• W2560084685 sameAs 2560084685 @default.
• W2560084685 citedByCount "13" @default.
• W2560084685 countsByYear W25600846852018 @default.
• W2560084685 countsByYear W25600846852019 @default.
• W2560084685 countsByYear W25600846852020 @default.
• W2560084685 countsByYear W25600846852021 @default.
• W2560084685 countsByYear W25600846852023 @default.
• W2560084685 crossrefType "journal-article" @default.
• W2560084685 hasAuthorship W2560084685A5013850494 @default.
• W2560084685 hasAuthorship W2560084685A5052892649 @default.
• W2560084685 hasAuthorship W2560084685A5064119420 @default.
• W2560084685 hasConcept C11872896 @default.
• W2560084685 hasConcept C127313418 @default.
• W2560084685 hasConcept C151730666 @default.
• W2560084685 hasConcept C17409809 @default.
• W2560084685 hasConcept C2778849375 @default.
• W2560084685 hasConcept C33757491 @default.
• W2560084685 hasConcept C34122518 @default.
• W2560084685 hasConcept C42787717 @default.
• W2560084685 hasConcept C44938399 @default.
• W2560084685 hasConcept C57016615 @default.
• W2560084685 hasConcept C67236022 @default.
• W2560084685 hasConcept C77928131 @default.
• W2560084685 hasConcept C79572550 @default.
• W2560084685 hasConcept C79605941 @default.
• W2560084685 hasConceptScore W2560084685C11872896 @default.
• W2560084685 hasConceptScore W2560084685C127313418 @default.
• W2560084685 hasConceptScore W2560084685C151730666 @default.
• W2560084685 hasConceptScore W2560084685C17409809 @default.

• next