华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论

林伟, 王军, 刘飞, 冀文斌, 王清晨. 2013. 华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论. 岩石学报, 29(5): 1791-1810.
引用本文: 林伟, 王军, 刘飞, 冀文斌, 王清晨. 2013. 华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论. 岩石学报, 29(5): 1791-1810.
LIN Wei, WANG Jun, LIU Fei, JI WenBin, WANG QingChen. 2013. Late Mesozoic extension structures on the North China Craton and adjacent regions and its geodynamics. Acta Petrologica Sinica, 29(5): 1791-1810.
Citation: LIN Wei, WANG Jun, LIU Fei, JI WenBin, WANG QingChen. 2013. Late Mesozoic extension structures on the North China Craton and adjacent regions and its geodynamics. Acta Petrologica Sinica, 29(5): 1791-1810.

华北克拉通及邻区晚中生代伸展构造及其动力学背景的讨论

  • 基金项目:

    本文受国家973研究计划(2009CB825008);国家自然科学基金项目(41225009)和国家科技重大专项项目(2011ZX05008-001)联合资助.

详细信息
    作者简介:

    林伟,男,1968年生,构造地质学专业,长期从事造山带韧性变形及相关的构造解析工作,E-mail: linwei@mail.iggcas.ac.cn

  • 中图分类号: P542

Late Mesozoic extension structures on the North China Craton and adjacent regions and its geodynamics

  • 欧亚大陆东部晚中生代伸展构造十分显著,表现为大量发育的变质核杂岩、同构造岩浆岩、韧性拆离断层带等伸展成因的穹隆和地堑-半地堑盆地。通过对这些伸展构造进行系统分析、归纳和总结,将欧亚大陆东部晚中生代伸展构造发育区划分为:泛贝加尔-鄂霍次克带、华北西部带、华北东部带、华北南缘及秦岭-大别带和华南内陆带。这些伸展构造记录了大区域上的NW-SE方向伸展,构成了全球最大的陆壳伸展地区。这些伸展构造使地壳深部的岩石沿拆离断层折返至地表,从而使中下地壳结构发生了强烈的改造。除华北东部带给出了一个较为宽泛的伸展时段外,各个研究区所涉及的伸展穹隆及其相关的拆离断层所表现的伸展峰期时间均十分相近:位于130~126Ma之间。岩石圈根部的拆沉可能是这个巨型伸展构造带形成的动力学机制。这个模型为探讨华北克拉通破坏和减薄的时限、机制、模式及深部动力学背景提供直接的构造证据。

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  • 图 1 

    欧亚大陆东部晚中生代伸展构造图(据Lin et al., 2013a修改, 各项相关数据的参考文献参见正文)

    Figure 1. 

    Setting and distribution of the Late Mesozoic extension at the eastern part of Eurasia continent (modified after Lin et al., 2013a)

    图 2 

    泛贝加尔-鄂霍次克带晚中生代伸展构造和穹隆冷却史及相关年代学展布图解

    Figure 2. 

    Tectonic setting, distribution and cooling paths of the Late Mesozoic extension at the Transbaikalia-Okhotsk belt

    图 3 

    华北东部和西部带晚中生代伸展构造和穹隆冷却史及相关年代学展布图解

    Figure 3. 

    Tectonic setting, distribution and cooling paths of the Late Mesozoic extension at the northern parts of North China Block

    图 4 

    华北南缘及秦岭-大别带和华南内陆晚中生代伸展构造和穹隆冷却史及相关年代学展布图解

    Figure 4. 

    Tectonic setting, distribution and cooling paths of the Late Mesozoic extension at the South margin of North China Block, Qinling-Dabie belt and South China Block

    图 5 

    欧亚大陆东缘120Ma左右古地理重建图解及晚中生代西太平洋地区洋壳产出量变化图解(据Engebretson et al., 1985; Northrup et al., 1995; Maruyama et al., 1997修改)

    Figure 5. 

    Paleogeographic reconstructions of the eastern margin of Eurasia continent around 120Ma and the oceanic crust growthing at the western part of Pacific during the Late Mesozoic and Cenozoic (modified after Engebretson et al., 1985; Northrup et al., 1995; Maruyama et al., 1997)

    图 6 

    横贯华北北部晚中生代伸展穹隆、岩浆作用及相关拉分盆地的模式剖面图(据Lin and Wang, 2006修改; 相关年代学资料的参考文献参见正文)

    Figure 6. 

    Schematic crustal scale section showing the regional Late Mesozoic extensional tectonics, magmatic dome, metamorphic core complexes and half basins in northern China Block (modified after Lin and Wang, 2006; geochronological measurements come from references that mentioned at the text)

    图 7 

    欧亚大陆东部晚中生代伸展构造及相关的年代学展布图(据Lin et al., 2013a修改; 相关年代学资料的参考文献参见正文)

    Figure 7. 

    Extensional structures (extensional dome, syntectonic plutons, detachment faults and basins) and their radiochronological ages in the eastern part of the Eurasian continent (modified after Lin et al., 2013a; geochronological measurements come from references that mentioned at the text)

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Late Mesozoic co桭数湲来?女???婡桬愠湴杯?????婮敳湩杯??卬???潣湴獯歮慩祣慳?呩???畨潥???慷湵摬…?椲‵?????のㄠ?慡??偩慦琬琠敎牅渠?慨湩摮?欠楡湮敤洠慴瑨楥捩?瀠潢汥慡牲楩瑮祧?潯普??慨瑥攠??敮獳潨穡潮椭捙?敮硳瑨敡湮猠楯潲湯?楥湮?捣漠湢瑥楬湴攺渠瑐慡汲?丠???猠楁慮??偯整牲獯灰敹挠瑯楦瘠敭獡?普牥潴浩?洠敳瑵慳浣潥牰灴桩楢捩?捩潴特攠?据潤洠灧汲敡硶敩獴??呭敯捤瑥潬湩楮捧献???の?????吠??びづ???摨漬椠?″ㄨ????祝??代???呲?がど?????扇牓?坡慮湤朠?呡???甠潇????娹核改渮朠?奨????潩湧獩歮愠祯慦?呭噥???汯慲摰歨潩捣栠畣扯????婯敭湰杬??卥???楮?????坡慣湨杭?奮??慦湡摵??慳稠畦歯慲扭穥潤瘠?????でㄠ???呴楩浡楲湹朠?慯湮摴?灮牥潮捴敡獬猠敥獸?潥普??慯瑮攠??攠獴潨穥漠楮捯?浴楨摥?汮漠睃敯牬?捲牡畤獯琠慒汩?敥硲琠敲湥獧楩潯湮?椠湕?捓漮湁琮椠湊敯湵瑲慮污?丠???獓楴慲?慣湴摵?楡浬瀠汇楥捯慬瑯楧潹測猠?昱漨爱?琲栩攺?琶攵挭琹漴渼楢捲 ̄獌敩瑵琠楃測朠?潥普?琠桊敆?搠敓獵琠牓畇挬琠楘潩湡?漠晑?琬栠敌?乯漠牚瑈栬??桡楮湧愠??爠慡瑮潤渠???慌楑渮氠礲‰挰漴渮猠瑚物慲楣湯敮搠?扈祒?積楐爠捤潡湴?啮?倠扯?愠杙敵獮?晥牮潧浳?浡敮琠慧浮潥物灳桳楩捣?捧潲牡敮?捴潥洠灡汮敤砠敩獴???楥瑯桬潯獧???????????????扣牥?圠慁湣杴?堠???乲敯畬扯慧畩散牡?????敩湮獥敲牡???慩湣摡?夠愲渳木′圩????????吶栠攨??愠扃楨敩?啥?健?畷湩楴瑨???敧湬瑩牳慨氠??桳楴湲慡?????牲放瑌慩捵攠潊界猬?敄硡瑶敩湳猠楇漬渠慌汩?愠汚汙漠捡桮瑤栠潗湵?獆留瀮攠爲瀰漰猵攮搠?潨湥?慌?呡牯楮慡獮猠業捥?潡牭潯杲数湨??吠散牯牲慥?乣潯癭慰???????????ち?????戠牌?坡慯湮杩?塧匠?慲湯摶?婮档敥測朠?奯???㈠ぃと????猠畁瀠??に??獹甠灣??牴??獢畵灴?????猠畃灲??牡??杯敵??潲湯獴瑡牴慩楯湮琠獯?漠湥?瑳桴敥?摮甠捌瑩楡汯敮?摮敧昬漠牋浯慲瑥楡漠湡?潤映?瑯桮整?摧敵瑯慵捳栠浡敲湥瑡?献礠獔瑥散浴?潮景?瑨桹敳??潳甬稠椴搰椷愨渱?挲漩爺攠?挵漭洸瀰氼敢硲??獩潵甠瑊桌攬爠湇??桮椠晈敍測朠???桍椠湡慮???敵漠汌漮朠椲挰愰氶?删敌癡楴敥眠??????????????????楩湣??桯楲湥攠獣敯?睰楬瑥桸??渺朠汎楥獷栠?慯扮獳瑴牲慡捩瑮??戠牯?圠慬湩杴?奯?慰湨摥??椠??????ので????湎楯瑲楴慨氠?晨潩牮浡愮琠楐潲湯?慲湥摳?洠敩獮漠穎潡楴捵?瑡敬挠瑓潣湩楥据?敥砬栠由洶愨琱椩漺渠′漱昭′愶渠?楩湮琠牃慨捩潮湥瑳楥温攼湢瑲愾汌?琠敆捘琬漠湚楨捥?执攠汊瑐?漠晌?琠桗敐?渠潃牨瑥桮攠牍湈?灡慮牤琠?潨晥?瑧栠敚?吮愠椲栰愰渰朮??潨略渠瑭慡楩湮?扥敶汯瑬??敩慯獮琠数牡湴??獲楮愠??吠桐敨??潥畲牯湺慯汩?漠晭??整潬汥漠杩祮??????????????????戺爠?坨慥渠朧?奵??婲桯潯畭??奬?慵湤搧??楯??奬???ち??扨???湩瑥牮慣捥漠湆瑲楯湮整湩瑥慲汳?猠男瀨攱爩椺洠瀹漷猭攱搱?琠攨捩瑮漠湃楨捩獮????捷慩獴敨?獅瑮畧摬祩?楨渠?瑢桳整?坡散獴琩攼牢湲 ̄?楡汲汵獹?潭晡??攬椠橉楳湯杺??敩愠獙琬攠牋湩??桲楡渠慇???敤漠汔潥杲楡换慡汹?即潨捩椠敍琮礠?漹昹??洠敐牡楬捥慯??畯汧汲敡瑰楨湩??????????????????の???戠牉?坬慡湮杤?夺????慴湥?坴???偯敮湩杣?味偹??婨桥慳湩杳????慭渠搷‵?畍潡?????とづ???乥慳瑥畮牴攮?潉晳?瑡桮敤??敲獣漬稠漶椨挱?氺椠琱栲漱猭瀱栴攲爼楢捲 ̄浍慡湺瑵汫敡?慺湯摶?瑁敍挬琠潄湯楮捳?摡敹捡漠畔灖氬椠湇杬?扤敫湯散慨瑵桢?瑄桐攬??慫扬楹敡?佯牶漠杅敖測???敮湯瑭牡慲汣??桫椠湖慁???癤椠摓敡湬挧敮?晫牯潶浡??獂甮瀠?????猠畓灴??牣??獲略瀠?????獧略瀠??爠?杨敥漠捭桥牴潡湭潯汲潰杨祩??散汯敲浥攠湣瑯慭汰?慥湸搠?卦爠?乨摥?偂扵?楧獵潴瑵潩瀠楲捩?捧潥洠瀨潳獯極瑴楨潷湥獳?潥晲??慔牲污祮??牡敩瑫慡捬攠潲略獧?浯慮昩椮挠?楯杫湬敡潤畹猠?牡潲捴歨猠???桥敮浣楥捳愬氠??攷漨氱漩机礠??代木????????????????扶爠?坍愬渠杇?奡卤??塣楨慵湢朠??圬??婯桮畳???慡渠摔??椠慓湫杬??婲??㈠ぅ??挠??印瑰爠畇捓琬甠牉慺汢?慯湤摩?朠敉潁挬栠牗潡湮潧氠潔朠楡据慤氠?敥癮楧搠敌湓挮攠′昰漱爱??慔牨汥礠??牬敥瑮慧捡攠潍略獴?潭牯潲杰敨湩?瀠慃牯慲汥氠敃汯?数硬瑥數渠猨楗潥湳?潥晲?琠桔敲?摮畳换瑡楩汫敡?汩楡瑮栠潒獥灧桩敯牮攩?椠湄?瑫桬敡?湹漠牅瑡桲整牨渠??慩扥楮散?潳爬漠朴攴渰椨挱?戺攠氱琲?′?愱猲琱‵?桢楲渾慍???漠畑牒渮愠氲‰漰昳?匠瑗牨畡捴琠畤牲慯汶??敌潡汴潥朠祍???????????????は?戠牯?圠慴湨来?婮??慴湨摥?婮栠慃湨杩??堭?????????整瑲慡浣潴爿瀠桔楥捣?捯潮牯数?捩潹浳灣汳攬砠″椶渹?堳椭漴温机?攱爵猵栭愱渷?愼湢摲 ̄瑍桥敮?愠摑癒愬渠捈敵猠?楍測?灊物潮猠灊救挬琠楚湨条???教漠污潮杤椠捘慵氠??砮瀠氲漰爰愳琮椠潔湥?晴潯牮?乣潳渠?晦攠牴牨潥甠獌??敥琠慍汥獳?????????????????楩湯??桬椠湢敡獳敩?眠楳瑹桳??湭朠汩楮猠桴?慥戠獃瑨物慮捡琭??扮牧?坬慩瑡猠潢湯??健???慥祧睩慯牮搮?????偮愠牒步楳湥獡潲湣??丠?愵渨搳?娺栠愳渹朷?娴?????????偺汩慥瑳攠?瑁攬挠瑆潡湮椠捗?栬椠獡瑮潤爠祚??扮慧猠楍渮?搱改瘹攳氮漠灐浡敬湡瑥?慺湯摩?瀠敡瑮牤漠汃敥畮浯?獯潩畣爠捬敩?牨潯捰歲?摢敥灳漠獡楮瑤椠潴湨?漠湬獯桳潳爠敯??栾椱渲愰???慯牦椠湁敲?慨湡摥?偮攠瑬物潴汨敯畳浰??敲潥氬漠杓祩????????????????戬爠?坨敩扮扡??????牐慲桩慣浨?卲????漬栠湁獬潡湢??????慔搬愠版捡桲???愬渠摎??攠湡摮牤椠硎??卲????????佳挮挩甮爠牍敡湧捭敡??慣朠敐??慣湥摳?楥浳瀠污楮捤愠瑐楬潡湴獥?潔晥?瑴桯敮?奣慳朮愠湇?佯湬捯桧??慡祬爠桓慯湣?浥整瑹愠浯潦爠灌桯楮捤?据漬爠敓?捥潣浩灡汬攠硐??獬潩畣瑡桴敩牯湮??漷渶机漠氷椱愭???敢潲氾潍来祮?????????????????戮爠?圹甹??夠?慥湯摤?卮畡湭??女????????呎桯敲??攠獃潨穩潮楡挠?浲慡杴浯慮琮椠獉浮?愠湆摬?汷楥瑲栠潍獆灊栬攠牃楨捵?瑧栠楓湌測椠湌杯?楃湈?敡慮獤琠敌牥湥??桙椠渨慥???漩甮爠湍慡汮?潬晥??桹慮湡杭捩档畳渠?啮湤椠癐敬牡獴楥琠祉?潴晥?卡捣楴敩湯据敳?慩湮搠?呡敳捴栠湁潳汩潡本礠??????????????????椮渠??桳楨湩敮獧整?睮椺琠桁??湲杩汣楡獮栠?慥扯獰瑨特慳捩瑣??戠牕?坩畯??夠??区甠渱‵?夭??娵格慢湲朾????慨湲摵?删敃湊?堠坒???づの????敡敮灤?杂敵潲摣票湦慩浥楬挠獂?漮映?夹愹渵献栠慍湯??潯癮攠浯敦渠瑴???敐潡汣潩杦楩捣愠汰??潴略爠湲慥汬?潴晩??栠楴湯愠?啵湲楡癳敩牡猠楡瑮楤攠獩?????????????????楴湩??栠楴湯攠獃敥?睯楺瑯桩??湥杸汴楥獮桳?慯扮猠瑡牬慯据瑧??扨牥?坥畡??奥???敭?坲???匠畯湦??奵?慡湳摩??甠潇????????????椩猺挠男猱猹椭漷渲猲?潢湲 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̄呕桮敯?呋教挬琠潏湴楯捦??癩漠汔甠瑡楮潤渠?潡晴??獤楡愮??丹改眹?夠潌牡歴???慲浥扴牡楣摥杯敵?唠湰楡癬敥牯獭楡瑧祮?側物散猠獲??????????扭爠?奨略??乯??奨敥????慁湳摩?偮攠湣杯??卩????????剡敲汧慩瑮椺漠湔獨桥椠灓?扫敨瑯睴敥攠湁?瑩桮攠??慵祮畴湡獩桮愠湲?浮敧瑥愬洠潥牡灳桴楥捲?挠潒牵敳?捩潡洮瀠汇敥硯?慨湹摳?浣楡湬攠牒慥汳楥穡慲瑣楨漠湌??呴慥潲汳椬渠???甠渵愵渳?倵爵漶瘼楢湲挾敖???敤潥琠敂捥瑥潫渠楐捁愬?敄瑥??敡瑵慸氠汄漬朠敁湮楤慥????????????????楌湥??栠楋湇攮猠攱?眹椶琮栠??湲杬汹椠獃桲?慴扡獣瑥牯慵捳琠??扮牵?婡桴慩楯?????婡桴略?删奴???楯畮??????整渠杴?兣剴???潣畳?兩????略?卂????楬?婲??婩桯慮測朠????慩湢摥??楡甮?坊???のち???呦椠浴敨?爠慇湥杯敬?潧晩??敬猠潓穯潣楩捥?瑹攬挠琱漵渳椺挠‵爱攵札椵洲攳?楢湲瘾敗牡獮楧漠湐?椬渠?敩慵猠瑚敊爬渠?乡潮牧琠桓??桡楮湤愠?扯汮潧挠歗??匠挲椰攰渲挮攠?楳湵??栴椰渼愯??印放牁楲支猼????″?????? ̄??ㄠ????K/Ar dating on the volcanic rocks in the Songliao basin, NE China: Constraints on stratigraphy and basin dynamics. International Journal of Earth Sciences, 91(2): 331-340

     

    Wang T, Zheng YD, Li TB and Gao YJ. 2004. Mesozoic granitic magmatism in extensional tectonics near the Mongolian border in China and its implications for crustal growth. Journal of Asia Earth Science, 23(5): 715-729

     

    Wang T, Zheng YD, Zhang JJ, Wang XS, Zeng LS and Tong Y. 2007. Some problems in the study of Mesozoic extensional structure in the North China craton and its significance for the study of lithospheric thinning. Geological Bulletin of China, 26(9): 1154-1166 (in Chinese with English abstract)

     

    Wang T, Z

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出版历程
收稿日期:  2013-02-10
修回日期:  2013-04-13
刊出日期:  2013-05-01

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