FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2528077978> ?p ?o ?g. }

• W2528077978 endingPage "1798" @default.
• W2528077978 startingPage "1783" @default.
• W2528077978 abstract "With many new discoveries of giant Mo deposits in the past decade, northeastern China has become the largest molybdenum mineralization region in China. The Xilamulun district is in the southern part of northeastern China and contains 25 Mo deposits and prospects, dominantly of porphyry type. These deposits are mostly along the E-striking Xilamulun fault. Re-Os dating of hydrothermal molybdenite from four deposits in the northern Xilamulun district revealed mineralization ages of 137 to 129 Ma (129.4 ± 3.4 Ma for Aolunhua, 135.3± 2.6 Ma for Shabutai, 136.4 ± 0.8 Ma for Haisugou, and 136.1 ± 6.6 Ma for Banlashan), in general agreement with the crystallization ages of their host granitoids.The compilation of existing data on Mo-bearing deposits in northeastern China, including the new data of this study, shows that Mesozoic Mo deposits in this region have a wide range of ages, from ~250 to 90 Ma. We propose that they are linked to three tectonic-magmatic events: (1) Triassic Mo deposits (250–220 Ma) are mainly distributed along the E-trending Xilamulun fault and are related to postcollisional crustal extension following the final closure of the Paleo-Asian ocean; (2) Jurassic Mo mineralization (200–140 Ma) displays a clear younging trend from southeast to northwest, coincides with the regional magmatism trend, and is interpreted to be related to the northwestward flat-slab subduction of the Paleo-Pacific plate beneath the Eurasian continent that started in the Early Jurassic (ca. 200 Ma); (3) Cretaceous Mo mineralization (140–90 Ma) shows a reversed migration trend from northwest to southeast, and can be explained by the coastward migration of slab rollback related to lower crust delamination, asthenospheric upwelling, and lithospheric thinning in eastern China. The spatial-temporal distribution of Mesozoic Mo mineralization is important for regional metallogeny and exploration. Recently numerous epithermal Au (Cu, Mo) deposits have been recognized in the southeast margin of northeastern China. According to this study, we predict that hidden porphyry/skarn systems could be located beneath these epithermal deposits." @default.
• W2528077978 created "2016-10-14" @default.
• W2528077978 creator A5005919986 @default.
• W2528077978 creator A5019872030 @default.
• W2528077978 creator A5038025885 @default.
• W2528077978 creator A5047273213 @default.
• W2528077978 creator A5058611234 @default.
• W2528077978 creator A5076279749 @default.
• W2528077978 date "2016-10-07" @default.
• W2528077978 modified "2023-10-06" @default.
• W2528077978 title "Regional Metallogeny of Mo-Bearing Deposits in Northeastern China, with New Re-Os Dates of Porphyry Mo Deposits in the Northern Xilamulun District" @default.
• W2528077978 cites W120028556 @default.
• W2528077978 cites W1497042339 @default.
• W2528077978 cites W1506904100 @default.
• W2528077978 cites W1751276650 @default.
• W2528077978 cites W1797283169 @default.
• W2528077978 cites W1892477717 @default.
• W2528077978 cites W1967437614 @default.
• W2528077978 cites W1967827341 @default.
• W2528077978 cites W1969296062 @default.
• W2528077978 cites W1971616481 @default.
• W2528077978 cites W1972349245 @default.
• W2528077978 cites W1975759160 @default.
• W2528077978 cites W1981367054 @default.
• W2528077978 cites W1982383011 @default.
• W2528077978 cites W1988557437 @default.
• W2528077978 cites W1991323502 @default.
• W2528077978 cites W1992068475 @default.
• W2528077978 cites W1992781439 @default.
• W2528077978 cites W1993716912 @default.
• W2528077978 cites W2001285983 @default.
• W2528077978 cites W2003954276 @default.
• W2528077978 cites W2004993774 @default.
• W2528077978 cites W2005781914 @default.
• W2528077978 cites W2006510222 @default.
• W2528077978 cites W2012556343 @default.
• W2528077978 cites W2019259962 @default.
• W2528077978 cites W2020224914 @default.
• W2528077978 cites W2021378803 @default.
• W2528077978 cites W2024998721 @default.
• W2528077978 cites W2025011208 @default.
• W2528077978 cites W2026313871 @default.
• W2528077978 cites W2028912811 @default.
• W2528077978 cites W2031839367 @default.
• W2528077978 cites W2032827575 @default.
• W2528077978 cites W2035003573 @default.
• W2528077978 cites W2037728688 @default.
• W2528077978 cites W2038677898 @default.
• W2528077978 cites W2041735999 @default.
• W2528077978 cites W2042878180 @default.
• W2528077978 cites W2045875839 @default.
• W2528077978 cites W2051829209 @default.
• W2528077978 cites W2052916443 @default.
• W2528077978 cites W2055668839 @default.
• W2528077978 cites W2056344831 @default.
• W2528077978 cites W2061118859 @default.
• W2528077978 cites W2063648931 @default.
• W2528077978 cites W2066128949 @default.
• W2528077978 cites W2067897273 @default.
• W2528077978 cites W2069359268 @default.
• W2528077978 cites W2072481433 @default.
• W2528077978 cites W2072680255 @default.
• W2528077978 cites W2075771303 @default.
• W2528077978 cites W2077214987 @default.
• W2528077978 cites W2081241828 @default.
• W2528077978 cites W2082270747 @default.
• W2528077978 cites W2086815595 @default.
• W2528077978 cites W2086889116 @default.
• W2528077978 cites W2093326692 @default.
• W2528077978 cites W2100376263 @default.
• W2528077978 cites W2103040999 @default.
• W2528077978 cites W2111481519 @default.
• W2528077978 cites W2115176890 @default.
• W2528077978 cites W2121762712 @default.
• W2528077978 cites W2124294269 @default.
• W2528077978 cites W2130869872 @default.
• W2528077978 cites W2136349207 @default.
• W2528077978 cites W2137470957 @default.
• W2528077978 cites W2137714492 @default.
• W2528077978 cites W2154141422 @default.
• W2528077978 cites W2165394332 @default.
• W2528077978 cites W2181387605 @default.
• W2528077978 cites W2353572957 @default.
• W2528077978 cites W2357058069 @default.
• W2528077978 cites W2359049200 @default.
• W2528077978 cites W2359469728 @default.
• W2528077978 cites W2361974973 @default.
• W2528077978 cites W2362892092 @default.
• W2528077978 cites W2364674515 @default.
• W2528077978 cites W2364927895 @default.
• W2528077978 cites W2371480344 @default.
• W2528077978 cites W2373922286 @default.
• W2528077978 cites W2384846805 @default.
• W2528077978 cites W2389783155 @default.
• W2528077978 cites W2391358439 @default.
• W2528077978 cites W2391845081 @default.
• W2528077978 cites W243257521 @default.
• W2528077978 cites W2465606019 @default.

• next