小兴安岭东南晚奥陶世鹤林侵入杂岩体成因探讨

现代地质 ›› 2009, Vol. 23 ›› Issue (3): 497-507.

小兴安岭东南晚奥陶世鹤林侵入杂岩体成因探讨

韩振哲^1,2,3，赵寒冬^1,2,4，吕军^1,2,3，李娟娟³，李文龙³，王盘喜^1,2

1中国地质大学地质过程与矿产资源国家重点实验室，北京100083；2中国地质大学岩石圈构造、深部过程及探测技术教育部重点实验室，北京100083；3黑龙江省地质调查研究总院齐齐哈尔分院，黑龙江齐齐哈尔161005；4黑龙江省地质调查研究总院，黑龙江哈尔滨150036

收稿日期:2008-11-10 修回日期:2009-04-30 出版日期:2009-06-20 发布日期:2011-12-21
作者简介:韩振哲，男，高级工程师，博士研究生，1965年出生，矿物学、岩石学、矿床学专业，从事区域地质矿产调查及研究工作。E-mail：hzhenz65@163.com
基金资助:
中国地质调查局基础地质调查项目（200313000035）；国家自然科学基金项目（40672088）

Petrogenesis of the Late Ordovician Helin Intrusive Complex in the Southeastern Xiaoxinganling Mountains

HAN Zhen-Zhe^1,2,3，ZHAO Han-Dong^1,2,4， LV Jun^1,2,3，LI Juan-Juan³， LI Wen-Long³，WANG Pan-Xi^1,2

1State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing100083, China;2Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing100083, China;3Qiqihar Branch,Heilongjiang Institute of Geological Survey, Qiqihar, Heilongjiang161005, China;4Heilongjiang Institute of Geological Survey, Harbin, Heilongjiang150036, China

Received:2008-11-10 Revised:2009-04-30 Online:2009-06-20 Published:2011-12-21

摘要/Abstract

摘要：

小兴安岭东南晚奥陶世鹤林侵入杂岩体岩性变化较大，由角闪辉长岩—（石英）闪长岩—英云闪长岩—二长花岗岩组成，不同岩石类型在野外宏观上呈相互侵入、包裹和渐变的接触关系；在（石英）闪长岩、英云闪长岩和二长花岗岩中均发育微细粒闪长质包体，包体多具明显塑性流变特点的浑圆外形和典型岩浆结构、针状磷灰石及捕获的寄主岩钾长石、石英斑晶，为MME型岩浆混合成因包体；杂岩体相对富集LILE（Ba、Sr、Rb）、HFS（U、Th、Zr、Ce）元素等，显示出壳源特点，而较高的ε_Nd（t）值（-2.38~-3.77）显示以幔源为主的特点。研究表明杂岩体具明显的壳幔岩浆混合成因的岩相学、岩石化学和地球化学特征，形成于基性岩浆底侵作用下的陆缘弧型活动大陆边缘构造环境。

关键词: 岩浆侵入杂岩体, MME型包体, 岩浆混合成因, 小兴安岭东南, 晚奥陶世

Abstract:

The Late Ordovician Helin intrusive complex in the southeast of Xiaoxinganling Mountains consists of a series of different rocks，including amphibole gabbro，(quartz)diorite，tonalite and monzonitic granite. Intrusive, inclusive and gradual transitional contact relationship has been recognized among different rock types. Some microgranular dioritic enclaves have been discovered in(quartz）diorite, tonalite and monzonitic granite. The enclaves have mainly ovoidlike shape, possibly caused by plastic flow, typically magma structure, acicular apatite as well as K-feldspar and quartz phenocrysts of host rocks, indicating an origin of magma mingling enclaves(MME). The intrusive complex is characterized by enrichment of large ion lithophile elements LILE(Ba，Sr，Rb)and HFS (U，Th，Zr，Ce)relative to primitive mantle, suggesting derivation of crust. However relatively high ε_Nd（t）values（-2.38 to -3.77）reflects a mantlederived source. In summary, petrographic petrochemical and geochemical characteristics of the Helin complex suggest mixed crustmantle origin. It can be attributed to underplating of mafic magma in an active continent marginal arc setting.

Key words: magma intrusive complex, microgranitoid mafic enclave(MME), magma mingling, southeastern Xiaoxinganling Mountains, Late Ordovicia

中图分类号:

P588.12

韩振哲赵寒冬吕军李娟娟李文龙王盘喜. 小兴安岭东南晚奥陶世鹤林侵入杂岩体成因探讨[J]. 现代地质, 2009, 23(3): 497-507.

HAN Zhen-Zhe，ZHAO Han-Dong，LV Jun，LI Juan-Juan， LI Wen-Long，WANG Pan-Xi. Petrogenesis of the Late Ordovician Helin Intrusive Complex in the Southeastern Xiaoxinganling Mountains[J]. Geoscience, 2009, 23(3): 497-507.