| Citation: |
WANG Lianxun, MA Changqian, XIONG Fuhao, WANG Fukang, GUO Futao, LIU Jing. 2017: Geological mapping approach to hybrid type granitic batholiths:A case study of the Jialuhe complex from East Kunlun orogen. Geological Bulletin of China, 36(11): 1971-1986.
|
Mafic enclaves are widespread in the granitic rocks of Eastern Kunlun orogen. They provide essential evidence for mixing events of magmas from the mantle and the crust, and thus the Eastern Kunlun granite belt is considered to be a natural laboratory of magma mixing. In recent years, arguments appear in applying comagmatic granitical mapping method to hybrid type granitic batholiths in an orogen environment. In this paper, the authors studied the Jialuhe hybrid type granite complex from East Kunlun orogen, aiming to shed some new lights on mapping methods of hybrid type granites. Based on field work, petrography, mineral and rock chemistry information, it is concluded that the Jialuhe granodiorite and the mafic enclaves inside resulted from magma mixing event under open systems. During the work, the authors divided the igneous rocks into two supper units, i.e., hybrid unit and un-hybrid unit. Based on the theory of magma mixing, three sub-units were further established:mafic end-member, felsic end-member and hybrid products. The basic unit for end-member rocks is pluton according to differences in mineral assemblages and textures of rocks. Likewise, the hybrid products could be further divided into different mixing units based on the different degrees of mixing or on the variations of enclave distributions. This mapping method is somehow similar to the traditional comagmatic granitical mapping method, and provides a preliminary exploration scheme for mapping work of hybrid type granite batholiths.
|
高秉璋, 洪大卫, 郑基俭, 等.花岗岩类1:5万区域地质填图方法指南[M].武汉:中国地质大学出版社, 1991:33.
|
|
肖庆辉, 周玉泉.一种值得重视的花岗岩类岩基填图新方法[J].中国地质, 1985, (8):16-18. http://www.cnki.com.cn/Article/CJFDTOTAL-QZDZ199000005.htm
|
|
洪大卫.关于花岗岩区的区域地质调查的某些问题[J].中国区域地质, 1986, (2):157-162. http://www.cnki.com.cn/Article/CJFDTotal-ZQYD198602009.htm
|
|
洪大卫.试论华南花岗岩岩套(岩石序列)的划分原则和研究方法[J].中国区域地质, 1986, (3):193-203. http://www.cnki.com.cn/Article/CJFDTOTAL-HBDK501.005.htm
|
|
廖庆康.花岗岩区单元超单元填图方法简介[J].广西地质, 1991, 4(1):73-80. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=gxdz199101013&dbname=CJFD&dbcode=CJFQ
|
|
廖瑞君, 韩仲仁.关于花岗岩1:5万填图中的几个问题[J].中国区域地质, 1998, 17(3):307-310. http://www.cqvip.com/QK/95894X/199803/3127963.html
|
|
杨崇辉, 庄育勋, 王新社, 等.关于"侵入岩谱系单位填图方法"有关问题的讨论[J].地质论评, 2001, 17(5):483-486. http://d.wanfangdata.com.cn/Periodical/OA000006666
|
|
李永军, 高占华, 李英, 等.西秦岭温泉岩浆混合花岗岩的地球化学特征[J].地质地球化学, 2003, 31(4):43-49. http://www.cqvip.com/QK/94506X/200304/9024201.html
|
|
窦全成, 董琳, 曹德云, 等.造山带异源浆混花岗岩理论及方法研究[J].矿产与地质, 2008, 22(3):188-195. http://www.cqvip.com/QK/96866X/200803/28153922.html
|
|
张旗, 潘国强, 李承东, 等.花岗岩混合问题:与玄武岩对比的启示-关于花岗岩研究的思考之一[J].岩石学报, 2007, 23(5):1141-1152. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=...
|
|
王涛.花岗岩混合成因研究及大陆动力学意义[J].岩石学报, 2000, 16(2):161-168. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200002002&dbname=CJFD&dbcode=CJFQ
|
|
Castro A, Moreno-Ventas I, Rosa J D D L. H-type (hybrid) granitoids:a proposed revision of the granite-type classification and nomenclature[J]. Earth-Science Reviews, 1991, 31(3/4):237-253. https://www.sciencedirect.com/science/article/pii/001282529190020G
|
|
吴志亮, 庄凤良, 甫为民.阿尔泰南缘混合花岗岩的包体特征及地质意义[J].昆明理工大学学报(自然科学版), 1990, (4):1-5. http://www.cqvip.com/QK/92599B/199004/4001647032.html
|
|
富云莲, 任纪舜, 陈廷愚, 等.福建晋江地区混合花岗岩及浅粒岩的40Ar/39Ar同位素年龄测定[J].地质论评, 1989, 35(6):552-557. http://www.cqvip.com/qk/91067X/198906/16627.html
|
|
贾文.赤峰市喇嘛洞混合花岗岩的发现[J].内蒙古地质, 1999, (1):29-33. http://www.cqvip.com/QK/86912X/199901/67877719090146002.html
|
|
许文良, 王清海, 杨德彬, 等.蚌埠荆山"混合花岗岩"[J].中国科学:地球科学, 2004, 34(5):423-428.
|
|
郑培玺.绥中混合花岗岩组成特征及意义[J].地质论评, 2013, 59(21):143-144. http://www.doc88.com/p-9794154988588.html
|
|
张德全, 孙桂英.对混合花岗岩的质疑——论中国大别山地区天堂寨片麻状花岗岩的成因[J].地球学报, 1991, (1):147-158. http://www.oalib.com/paper/1558570
|
|
陈丹玲, 赖绍聪, 刘养杰.秦皇岛柳江盆地混合花岗岩的锆石UPb定年[J].西北大学学报:自然科学版, 2007, 37(2):277-281. http://www.cqvip.com/QK/95994X/201503/1005679134.html
|
|
万渝生.雌山混合花岗岩及有关岩石的副矿物组合、锆石特征及其地质意义[J].地质论评, 1987, 33(3):229-237. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198703003.htm
|
|
万渝生.山东雁翎关地区雌山混合花岗岩地球化学特征及其成因[J].岩石矿物学杂志, 1986, 3:203-211. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198400016136.htm
|
|
陈江峰.简单混合、AFC混合和花岗岩同位素数据解释[J].安徽地质, 1991, 1(1):19-27. http://www.cqvip.com/QK/87123X/199101/1005289565.html
|
|
康磊. 新疆西准格尔夏尔莆岩浆混合花岗岩体的研究[D]. 长安大学硕士学位论文, 2010: 1-77.
|
|
李永军, 赵仁夫, 刘志武, 等.关于造山带花岗岩类填图方法的讨论[J].华南地质与矿产, 2003, (1):1-6. http://www.cnki.com.cn/Article/CJFDTotal-HNKC200301000.htm
|
|
孙吉明, 马中平, 唐卓, 等.阿尔金南缘鱼目泉岩浆混合花岗岩LA-ICP-MS测年与构造意义[J].地质学报, 2012, 86(2):247-257. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201202005.htm
|
|
孙雨, 裴先治, 丁仨平, 等.东昆仑哈拉尕吐岩浆混合花岗岩:来自锆石U-Pb年代学的证据[J].地质学报, 2009, 83(7):1000-1010. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=...
|
|
马昌前, 杨坤光, 唐仲华, 等.花岗岩类岩浆动力学——理论方法及鄂东花岗岩类例析[M].武汉:中国地质大学出版社, 1994:1-120.
|
|
许志琴, 杨经绥, 李海兵, 等.造山的高原-青藏高原的地体拼合、碰撞造山及隆升机制[M].北京:地质出版社, 2007.
|
|
莫宣学, 罗照华, 邓晋福, 等.东昆仑造山带花岗岩及地壳生长[J].高校地质学报, 2007, 13(3):403-414. http://d.wanfangdata.com.cn/Periodical/gxdzxb200703010
|
|
刘成东, 莫宣学, 罗照华, 等.东昆仑壳幔岩浆混合作用:来自锆石SHRIMP年代学的证据[J].科学通报, 2004, 49(6):596-602. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200406018.htm
|
|
谌宏伟, 罗照华, 莫宣学, 等.东昆仑造山带三叠纪岩浆混合成因花岗岩的岩浆底侵作用机制[J].中国地质, 2005, 32(3):386-395. http://www.docin.com/p-1096870368.html
|
|
陈国超, 裴先治, 李瑞保, 等.东昆仑东段香加南山花岗岩基的岩浆混合成因:来自镁铁质微粒包体的证据[J].地学前缘, 2016, 23(4):226-240. http://www.cnki.com.cn/Article/CJFDTotal-DXQY201604023.htm
|
|
刘成东, 张文秦, 莫宣学, 等.东昆仑约格鲁岩体暗色微粒包体特征及成因[J].地质通报, 2002, 21(11):739-744. doi: 10.3969/j.issn.1671-2552.2002.11.009
|
|
李昌年.赣东北晚元古代港边岩浆混合杂岩体的区域地质调查及岩石学研究[J].华南地质与矿产, 2002, (3):9-18. http://www.cqvip.com/QK/91196A/200203/6955924.html
|
|
Didier J. Granites and their Enclaves[M]. Elsevier, Amsterdam, 1973:1-393.
|
|
Vernon R H. Restite, xenoliths and microgranitoid enclaves in granites[J]. Journal and Proceeding-Royal Society of New South Wales, 1983, 116(3):77-103. http://www.oalib.com/references/19274613
|
|
Didier J, Barbarin B. Enclaves and granite petrology[M]. Elsevier, Amsterdam, 1991:1-625.
|
|
Baxter S, Feely M.Magma mixing and mingling textures in granitoids:examples from the Galway Granite, Connemara, Ireland[J]. Mineralogy and Petrology, 2002, 76(1/2):63-74. https://www.researchgate.net/publication/226977223_Magma_mixing...
|
|
王晓霞, 王涛, 卢欣祥, 等.北秦岭老君山、秦岭梁环斑结构花岗岩岩浆混合的岩相学证据及意义[J].地质通报, 2002, 21(8/9):523-529. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=200208122&journal_id=gbc
|
|
Barbarin B. Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California:nature, origin, and relations with the hosts[J]. Lithos, 2005, 80(1):155-177. doi: 10.1007/s12594-011-0052-1
|
|
Hibbard M J. Textural anatomy of twelve magma-mixed granitoid systems[C]//Didier J, Barbarrin B Z. Enclaves and Granite Petrology. Developments in Petrology, 3. Amsterdam:Elsevier. 1991:431-444.
|
|
Malcolm J H, Textural anatomy of twelve magma-mixed granitoid systems[C]//Didier J, Barbarin B. Enclaves and Granite Petrology. Elsevier, Amsterdam, 1991:431-444.
|
|
刘成东.东昆仑造山带东段花岗岩岩浆混合作用[M].北京:地质出版社, 2008:78-103.
|
|
史洪峰. 东昆仑布尔汗布达山都兰印支期岩浆岩中斜长石对岩浆混合作用的启示[D]. 中国地质大学(武汉)学士学位论文, 2010: 1-49.
|
|
Vernon R H. Microgranitoid enclaves in granites-globules of hybrid magma quenched in a plutonic environment[J]. Nature, 1984, 309(5967):438-439. doi: 10.1038/309438a0
|
|
Cantagrel J M, Didier J, Gourgaud A. Magma mixing:origin of intermediate rocks and "enclaves" from volcanism to plutonism[J]. Physics of the Earth & Planetary Interiors, 1984, 35(1/3):63-76. https://www.researchgate.net/publication/223529825_Magma_mixing...
|
|
徐夕生, 范钦成, 蒋少涌, 等.安徽铜官山石英闪长岩及其包体锆石U-Pb定年与成因探讨[J].科学通报, 2004, 49(18):1883-1891. doi: 10.3321/j.issn:0023-074X.2004.18.012
|
|
王德滋.微粒花岗岩包体的成因[J].桂林冶金地质学院学报, 1992, (3):235-240.
|
|
马昌前, 王人镜, 邱家骧.花岗质岩浆起源和多次岩浆混合的标志:包体-以北京周口店岩体为例[J].地质论评, 1992, 38(2):109-119. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199202001.htm
|
|
青海地质局. 青海省加鲁河幅1: 20万区域地质图(Ⅰ-47-Ⅲ). 1973.
|
|
中国地质大学(武汉). 青海省冬给措纳湖幅1: 25万区域地质图(I47C001002). 2001.
|
Supported by: Beijing Renhe Information Technology Co., Ltd. 
DownLoad: