
第25卷第5期 2011年10月
现代地质 GFOSCIENCF
胶北地块前寒武纪基底研究新进展
徐扬2,冯岩”,李日辉12
(1.国土资源部海洋油气资源与环境地质重点实验室,山东青岛266071;
2.青岛海洋地质研充所,山东青岛266071;3.中国地质大学能源学院,北京100083)
Vol 25 No.5
Oet.2011
摘要:胶北地块位于鲁东的沂述断裂和五蓬一烟台断裂之间,以出露不同变质程度的太古宙一古元古代的结晶基底为特征,其岩石组合为TTC质(英云闪长岩-奥长花岗岩-花岗闪长岩)片麻岩和少量变质表壳岩(变质火山岩-变质沉积岩),它们构成了胶北的花岗-绿岩体。对变质(超)基性岩、TTG岩系的岩石组合、地球化学特征和同位素年代学的研究表明,胶北地块造壳的主要时期为新太古代的2.8~2.7Ga;在经历了2.5Ga左右构造事件后,胶北地块进人稳定陆壳沉积阶段,并接受了古元古代的孔慈岩系沉积;最后于1.8Ga左右发生变质。与苏鲁造山带不同,胶北地块前寒
武纪基底具有许多亲华北板块的特征,二者的界线可能是五莲一烟台断裂。关键调:TTG;变质(超)基性岩;前寒武纪基底:胶北地块
中图分类号:P548;P534.1
文献标志码:A
文章编号:10008527(2011)05-0965-10
MainProgressesintheStudyofPrecambrianBasementof
JiaobeiTerrane,EasternChina XU Yang"-, FENG Yan ", LI Ri-hui'.2
(1. Key Laboratory of Marine Hydrocarbon Resources and Entironmeslal Geology, Ministry of Land and Resources, Qingdao
Shandong 266071, China; 2. Qingdao Institule of Marine Geology, Qingdao, Shandong266071, China;
3. School of Energy Resources, China Unisersity of Ceoucienoes, Bejing 100083, China)
Abstract: The Jiaodong terrane located between Yishu fault and Wulian-Yantai fault in eastern Shandong Pro-vince, is characterized by an Archean to Paleoproterozoic crystalline basement experienced different degrees of metamorphism traditionally. Its assemblage includes TTG (tonalitic-trondhjemitic-granodioritic) gneisses and a little supracrustal rocks(metavolcanite and metasedimentary), which combined to granite-greenstone belts of Jiaodong terrane. The research of lithological, geochemical, geochronological data indicated that its continental crust was chiefly generated in Neoarchean (2. 8 2. 7 Ga), and then it started intracratonic deposit of Paleo-proterozoic khondalite after tectonic event at 2. 5 Ga, finally it undergone the metamorphic event at 1. 8 Ga. Different from Sulu orogen, some characteristics of Precambrian basement of Jiaobei terrane are related to North China Craton, and the boundary between them maybe locate along the Wulian-Yantai fault.
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1概述
胶莱盆地的中新生代碎屑沉积,西以沂沐断裂(郏庐断裂的北延)和华北的鲁西地块分隔,东部以五
胶北地块,也被称为胶北隆起,位于山东半莲一烟台断裂与苏鲁造山带相邻(图1)。由于大岛的北部,其北部濒临渤海湾和北黄海,南临近面积出露太古宙的古老岩石,使得胶北地块成为
收稿日期:2011-05-11;改回日期:2011~09-10;责任编辑:潘令枝。基金项目:国土资源部海洋区域地质调查项目(CZH200800501)。
作者简介:徐扬,男,研究实习员,1985年出生,构造地质学专业,主要从事构造地质学研究。
Email; xuyang_ 0112@ 163. com。