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• W2779741034 endingPage "189" @default.
• W2779741034 startingPage "178" @default.
• W2779741034 abstract "A study of teleseismic P-wave tomography was carried out along the Central Orogenic Belt of China (COBC) consisting of the Qinling, Tongbai, Hong'an, Dabie and Sulu orogens that were created by northward subduction of the South China Block beneath the North China Block to subarc depths in the Paleozoic to Mesozoic. The results show the presence of high velocity anomaly underneath the COBC and its adjacent cratonic regions but the absence of high velocity anomaly in the lower lithosphere beneath the COBC. The high velocity anomaly is deep underneath the COBC, possibly representing the relic of the subducted Paleo-Tethyan oceanic slab predating the continental deep subduction of the South China Block. The high velocity anomaly is also deep underneath the southeastern part of the North China Block, possibly being a relic of the subducted Paleo-Pacific slab. However, no relic of the deeply subducted continental slab is seismically detected in the lower lithosphere beneath the Dabie and Sulu orogens, though the occurrence of ultrahigh-pressure metamorphic rocks in the two orogens has clearly demonstrated continental deep subduction to subarc depths in the Triassic. Instead there is only the relatively flat and uniform Moho boundary beneath the COBC region, indicating that the subduction-thickened continental lithosphere along the COBC has lost its root. It is inferred that the orogenic root beneath the COBC region has been foundered into the asthenospheric mantle at the postcollisional stage. The foundering would have taken place in the Early Cretaceous as indicated by the extensive occurrence of magmatic and migmatitic rocks along the COBC. As a consequence, the seismic tomography cannot detect the deeply subducted continental slab remnant from the Triassic period. It is possible that the tomographic visibility of continental subduction in the lower lithosphere is limited to the past 100 Myr." @default.
• W2779741034 created "2018-01-05" @default.
• W2779741034 creator A5038855167 @default.
• W2779741034 creator A5088693838 @default.
• W2779741034 date "2018-01-01" @default.
• W2779741034 modified "2023-10-18" @default.
• W2779741034 title "Seismic evidence for the absence of deeply subducted continental slabs in the lower lithosphere beneath the Central Orogenic Belt of China" @default.
• W2779741034 cites W1526406511 @default.
• W2779741034 cites W1586411303 @default.
• W2779741034 cites W1588263366 @default.
• W2779741034 cites W1878752643 @default.
• W2779741034 cites W1891158109 @default.
• W2779741034 cites W1967921001 @default.
• W2779741034 cites W1975734686 @default.
• W2779741034 cites W1976967272 @default.
• W2779741034 cites W1978364492 @default.
• W2779741034 cites W1981344517 @default.
• W2779741034 cites W1990751086 @default.
• W2779741034 cites W1992248172 @default.
• W2779741034 cites W1992599763 @default.
• W2779741034 cites W1997310688 @default.
• W2779741034 cites W2001799257 @default.
• W2779741034 cites W2003311821 @default.
• W2779741034 cites W2003417910 @default.
• W2779741034 cites W2005521948 @default.
• W2779741034 cites W2013579065 @default.
• W2779741034 cites W2014364988 @default.
• W2779741034 cites W2016748354 @default.
• W2779741034 cites W2017572837 @default.
• W2779741034 cites W2024136716 @default.
• W2779741034 cites W2028327545 @default.
• W2779741034 cites W2028642961 @default.
• W2779741034 cites W2031604650 @default.
• W2779741034 cites W2033800529 @default.
• W2779741034 cites W2038538609 @default.
• W2779741034 cites W2038569126 @default.
• W2779741034 cites W2041352930 @default.
• W2779741034 cites W2042402279 @default.
• W2779741034 cites W2047230097 @default.
• W2779741034 cites W2051402121 @default.
• W2779741034 cites W2052584682 @default.
• W2779741034 cites W2053422899 @default.
• W2779741034 cites W2054267841 @default.
• W2779741034 cites W2058193023 @default.
• W2779741034 cites W2062578168 @default.
• W2779741034 cites W2063754919 @default.
• W2779741034 cites W2065092571 @default.
• W2779741034 cites W2066285517 @default.
• W2779741034 cites W2073203475 @default.
• W2779741034 cites W2073767751 @default.
• W2779741034 cites W2076039380 @default.
• W2779741034 cites W2078181124 @default.
• W2779741034 cites W2080918078 @default.
• W2779741034 cites W2083841543 @default.
• W2779741034 cites W2090446100 @default.
• W2779741034 cites W2092386709 @default.
• W2779741034 cites W2093036886 @default.
• W2779741034 cites W2093260086 @default.
• W2779741034 cites W2093554941 @default.
• W2779741034 cites W2097897435 @default.
• W2779741034 cites W2103113534 @default.
• W2779741034 cites W2105731467 @default.
• W2779741034 cites W2112191675 @default.
• W2779741034 cites W2112893827 @default.
• W2779741034 cites W2119666905 @default.
• W2779741034 cites W2120387369 @default.
• W2779741034 cites W2123481134 @default.
• W2779741034 cites W2126001268 @default.
• W2779741034 cites W2128624170 @default.
• W2779741034 cites W2139854519 @default.
• W2779741034 cites W2145056588 @default.
• W2779741034 cites W2161617180 @default.
• W2779741034 cites W2162591031 @default.
• W2779741034 cites W2165378552 @default.
• W2779741034 cites W2169985461 @default.
• W2779741034 cites W2257662574 @default.
• W2779741034 cites W2286069847 @default.
• W2779741034 cites W2299194302 @default.
• W2779741034 cites W2327395928 @default.
• W2779741034 cites W2333708872 @default.
• W2779741034 cites W2338345412 @default.
• W2779741034 cites W2393545348 @default.
• W2779741034 cites W2408707957 @default.
• W2779741034 cites W2509591576 @default.
• W2779741034 cites W2551198042 @default.
• W2779741034 cites W2554398624 @default.
• W2779741034 cites W2592090639 @default.
• W2779741034 cites W2592777846 @default.
• W2779741034 cites W2601277262 @default.
• W2779741034 cites W2606445678 @default.
• W2779741034 cites W2709636920 @default.
• W2779741034 cites W868724413 @default.
• W2779741034 doi "https://doi.org/10.1016/j.tecto.2017.12.018" @default.
• W2779741034 hasPublicationYear "2018" @default.
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