{"refrec":{"BRefID":256907,"RR":"<b>Mao, K.; Xie, X.; Xie, Y.; Ren, J.; Chen, H.</b> (2015). Post-rift tectonic reactivation and its effect on deep-water deposits in the Qiongdongnan Basin, northwestern South China Sea. <i>Mar. Geophys. Res. 36(2-3)</i>: 227-242. <a href=\"https://dx.doi.org/10.1007/s11001-015-9248-x\" target=\"_blank\">https://dx.doi.org/10.1007/s11001-015-9248-x</a>","BEntID":248916,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Mar. Geophys. Res. 36(2-3)</i>: 227-242. <a href=\"https://dx.doi.org/10.1007/s11001-015-9248-x\" target=\"_blank\">https://dx.doi.org/10.1007/s11001-015-9248-x</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Mao, K.; Xie, X.; Xie, Y.; Ren, J.; Chen, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Mao, K. <i>et al.</i>","Englishabstract":"The post-rift evolution of extensional basins is traditionally thought to be dominated by thermal subsidence due to cessation of the major fault activity during the post-rift stage. The Qiongdongnan Basin, which is located in the northwestern continental margins of the South China Sea, has exhibited significant deviations from typical post-rift characteristics. In the basin, a distinct tectonic reactivation occurred since the Late Miocene (11.6 Ma). Three notable aspects of the observed tectonic reactivation during the post-rift stage include, (1) pre-existing fault reactivation, (2) multiple large-scale magmatic intrusions, and (3) rapid post-rift subsidence. During this period the basin infill significantly changed in depositional environments shifting rapidly from littoral-neritic to bathyal-abyssal environments since Late Miocene. The pre-existing fault activity along the No. 2 fault of the basin resulted in the formation of initial shelf breaks and led to the development of continental slope. In addition, the pre-existing faults along the Central Depression zone created a small sub-basin with distinctive axial negative topography characteristics formed between structural highs. These geomorphological changes led to the formation of the Central Canyon. Large-scale magmatic intrusions occurred along the fault zone in the Central Depression of the basin during the post-rift stage. Those deviations, as evidenced from pre-existing fault reactivation, magmatic intrusions, and rapid post-rift subsidence in the Qiongdongnan Basin is believed to be related to the Hainan Plume event.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Post-rift tectonic reactivation and its effect on deep-water deposits in the Qiongdongnan Basin, northwestern South China Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-26 01:31:34.153668","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Post-rift stage; Tectonic reactivation; Pre-existing faults; Magmaticintrusion","OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2020-06-24","DateCreate":"2016-05-29","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000356605400011","VABBcode":null,"OpenAcc":0,"DOI":"10.1007/s11001-015-9248-x"},"refs":null,"anarec":{"AnaID":256907,"PubliDate":2015,"Pagination":"227-242","XtraPublOfAnaID":null,"ISBN":null,"Volume":"36","Issue":"2-3","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43366,"SerRR":"Marine Geophysical Researches. Reidel: Dordrecht.  ISSN 0025-3235; e-ISSN 1573-0581","StandardTitleSer":"Marine Geophysical Researches","ISSN":"0025-3235","AbbrevSer":"Mar. Geophys. 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