FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2568656431> ?p ?o ?g. }

• W2568656431 endingPage "140" @default.
• W2568656431 startingPage "109" @default.
• W2568656431 abstract "South China hosts the most abundant and largest tungsten (W) deposits in the world, being a famous W metallogenic region. Located at the eastern part of the South China Block, which was formed by amalgamation of the Yangtze and Cathaysia Blocks during the Neoproterozoic, these W deposits were mainly formed during the Mesozoic. The W mineralization is dominanted by greisen, quartz-vein, skarn, and porphyry types, all of which are genetically related to the evolution of highly fractionated granitoids. Four episodes of W mineralization are recognized: (1) Late Triassic (230–210 Ma) in the central and western parts of South China; (2) Middle Jurassic (ca. 170 Ma) to Early Cretaceous (ca. 140 Ma) in the interior of South China, with the mineralization being concentrated in southern Jiangxi Province between 165 and 150 Ma; (3) Early Cretaceous (136–120 Ma) with deposits across South China; and (4) Late Cretaceous (100–80 Ma) mainly in the southwestern parts of South China. These four periods of mineralization are closely related to the closure of paleo-Tethys and subduction of the paleo-Pacific plate. In the Late Triassic, these two events caused local extensional environments, facilitating emplacement of the peraluminous granitoids, and formation of the W deposits. In the Middle Jurassic, break-off of the subducting oceanic plate resulted in emplacement of highly fractionated granites in the Nanling region. Later anticlockwise rotation of the paleo-Pacific plate created widespread S-type granitoids and associated Middle Jurassic to Early Cretaceous W mineralization in the interior of South China. Since 136 Ma, rollback of the subducting Pacific plate resulted in weak W mineralization across South China. Finally, a change of direction in the retreating plate from SE to ESE resulted in intensive mineralization of the southwestern part of South China." @default.
• W2568656431 created "2017-01-13" @default.
• W2568656431 creator A5000273221 @default.
• W2568656431 creator A5013503446 @default.
• W2568656431 creator A5018459086 @default.
• W2568656431 creator A5044875459 @default.
• W2568656431 creator A5082651070 @default.
• W2568656431 date "2017-04-01" @default.
• W2568656431 modified "2023-10-14" @default.
• W2568656431 title "Genetic types, mineralization styles, and geodynamic settings of Mesozoic tungsten deposits in South China" @default.
• W2568656431 cites W130251069 @default.
• W2568656431 cites W1491765701 @default.
• W2568656431 cites W1514900759 @default.
• W2568656431 cites W1525258218 @default.
• W2568656431 cites W1572418335 @default.
• W2568656431 cites W1757959485 @default.
• W2568656431 cites W1850129459 @default.
• W2568656431 cites W1850405120 @default.
• W2568656431 cites W1965749890 @default.
• W2568656431 cites W1965840024 @default.
• W2568656431 cites W1966479677 @default.
• W2568656431 cites W1966642168 @default.
• W2568656431 cites W1968583876 @default.
• W2568656431 cites W1969185593 @default.
• W2568656431 cites W1969262468 @default.
• W2568656431 cites W1973219404 @default.
• W2568656431 cites W1974550974 @default.
• W2568656431 cites W1974569905 @default.
• W2568656431 cites W1974616352 @default.
• W2568656431 cites W1974895125 @default.
• W2568656431 cites W1975956926 @default.
• W2568656431 cites W1977795491 @default.
• W2568656431 cites W1980463640 @default.
• W2568656431 cites W1980884417 @default.
• W2568656431 cites W1981760759 @default.
• W2568656431 cites W1982272146 @default.
• W2568656431 cites W1983131682 @default.
• W2568656431 cites W1986934005 @default.
• W2568656431 cites W1987395670 @default.
• W2568656431 cites W1987759514 @default.
• W2568656431 cites W1991520358 @default.
• W2568656431 cites W1991862283 @default.
• W2568656431 cites W1994625967 @default.
• W2568656431 cites W1996489529 @default.
• W2568656431 cites W1999214300 @default.
• W2568656431 cites W1999609683 @default.
• W2568656431 cites W2000219006 @default.
• W2568656431 cites W2000275752 @default.
• W2568656431 cites W2000292276 @default.
• W2568656431 cites W2001034959 @default.
• W2568656431 cites W2001119618 @default.
• W2568656431 cites W2002424706 @default.
• W2568656431 cites W2002694143 @default.
• W2568656431 cites W2002947230 @default.
• W2568656431 cites W2003954276 @default.
• W2568656431 cites W2006981888 @default.
• W2568656431 cites W2008591861 @default.
• W2568656431 cites W2010435429 @default.
• W2568656431 cites W2010623866 @default.
• W2568656431 cites W2011548702 @default.
• W2568656431 cites W2012531754 @default.
• W2568656431 cites W2012942710 @default.
• W2568656431 cites W2012991210 @default.
• W2568656431 cites W2013747430 @default.
• W2568656431 cites W2013803090 @default.
• W2568656431 cites W2013810995 @default.
• W2568656431 cites W2015961036 @default.
• W2568656431 cites W2016872327 @default.
• W2568656431 cites W2017448452 @default.
• W2568656431 cites W2018490520 @default.
• W2568656431 cites W2019618011 @default.
• W2568656431 cites W2020529667 @default.
• W2568656431 cites W2020810837 @default.
• W2568656431 cites W2021940213 @default.
• W2568656431 cites W2024331643 @default.
• W2568656431 cites W2024338689 @default.
• W2568656431 cites W2024427164 @default.
• W2568656431 cites W2025576610 @default.
• W2568656431 cites W2025597990 @default.
• W2568656431 cites W2030713284 @default.
• W2568656431 cites W2032358291 @default.
• W2568656431 cites W2034383015 @default.
• W2568656431 cites W2034672517 @default.
• W2568656431 cites W2035988508 @default.
• W2568656431 cites W2037913789 @default.
• W2568656431 cites W2037941752 @default.
• W2568656431 cites W2038194848 @default.
• W2568656431 cites W2039226804 @default.
• W2568656431 cites W2039323682 @default.
• W2568656431 cites W2039324475 @default.
• W2568656431 cites W2039940511 @default.
• W2568656431 cites W2043612496 @default.
• W2568656431 cites W2045409783 @default.
• W2568656431 cites W2050203573 @default.
• W2568656431 cites W2051805987 @default.
• W2568656431 cites W2057898352 @default.
• W2568656431 cites W2058019619 @default.
• W2568656431 cites W2058314706 @default.

• next