喀喇昆仑天文点地区辉长岩锆石U-Pb年代学、地球化学特征及其构造意义
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摘要
新疆喀喇昆仑天文点地区广泛发育基性岩体,呈岩株状产出,岩性单一,主要由辉长岩和辉绿岩组成。采用LA-ICP-MS锆石U-Pb同位素定年法,获得辉长岩206Pb/238U加权平均年龄为(105±4) Ma,属早白垩世晚期。地球化学数据显示:岩石具有较低的SiO_2(44. 69%～48. 54%),较高的Al_2O_3(13. 6%～17. 66%)和CaO(7. 77%～11. 04%)含量以及较高的Mg#。稀土总量中等(∑REE=78. 57×10~(-6)～119. 3×10~(-6)),轻重稀土元素分异较为明显[(La/Yb)N=4. 28～5. 72],弱的正铕异常(δEu=1. 04～1. 27)。岩石相对富集大离子亲石元素Rb、Ba、K,Pb明显正异常,轻度亏损高场强元素Nb、P、Zr等。微量元素地球化学特征显示岩浆起源于过渡型地幔的部分熔融,并且在上升侵位过程中发生明显的地壳混染。天文点一带辉长岩具有板内玄武岩的地球化学特征,综合认为其形成于陆内伸展体制,结合前人研究成果,认为新特提斯洋盆早白垩世晚期已经闭合,区内进入后碰撞伸展阶段。
The intensively developed mafic intrusions with single lithology occuring as stocks in Tianwendian region of the Karakorum Mountains consist of gabbro and diabase.. The LA-ICP-MS zircon U-Pb dating of the Tianwendian gabbro yields an age of 105±4Ma,belonging to the late stage of the Early Cretaceous. Geochemical data indicate that the gabbros are low in SiO_2( 44. 69% ～48. 54%),high in Al_2O_3( 13. 6% ～ 17. 66%),CaO( 7. 77% ～ 11. 04%) and Mg#value. They have medium REE( ∑REE = 78. 57×10~(-6)～ 119. 3×10~(-6)),the fractionation of light and heavy rare earth elements is obvious[( La/Yb)N= 4. 28 ～ 5. 72],and slightly Eu anomalies( δEu = 1. 04 ～ 1. 27). Those rocks with Pb positive anomaly are enriched in LILE and depleted in HFSE. Geochemical characteristics of trace elements indicate that those rocks originate from partial melting of the transitional mantle,with significant crustal contamination during ascending process. The gabbros in Tianwendian region have the similar geochemical characteristics to the intraplate basalts,therefore in comprehensive consideration,they are formed in an intra-continent extensional setting. Based on regional geology,we agree that the Neo-Tethys oceanic basin has closed in the late stage of the Early Cretaceous,and the Karakorum region stepped in the stage of post-collisional extension.
The intensively developed mafic intrusions with single lithology occuring as stocks in Tianwendian region of the Karakorum Mountains consist of gabbro and diabase.. The LA-ICP-MS zircon U-Pb dating of the Tianwendian gabbro yields an age of 105±4Ma,belonging to the late stage of the Early Cretaceous. Geochemical data indicate that the gabbros are low in SiO_2( 44. 69% ～48. 54%),high in Al_2O_3( 13. 6% ～ 17. 66%),CaO( 7. 77% ～ 11. 04%) and Mg#value. They have medium REE( ∑REE = 78. 57×10~(-6)～ 119. 3×10~(-6)),the fractionation of light and heavy rare earth elements is obvious[( La/Yb)N= 4. 28 ～ 5. 72],and slightly Eu anomalies( δEu = 1. 04 ～ 1. 27). Those rocks with Pb positive anomaly are enriched in LILE and depleted in HFSE. Geochemical characteristics of trace elements indicate that those rocks originate from partial melting of the transitional mantle,with significant crustal contamination during ascending process. The gabbros in Tianwendian region have the similar geochemical characteristics to the intraplate basalts,therefore in comprehensive consideration,they are formed in an intra-continent extensional setting. Based on regional geology,we agree that the Neo-Tethys oceanic basin has closed in the late stage of the Early Cretaceous,and the Karakorum region stepped in the stage of post-collisional extension.
引文
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陈玉禄,江元生.2002.西藏班戈-切里错地区早白垩世火山岩的时代确定及意义[J].地质力学学报,8(1):43-49.
崔建堂,王炬川,边小卫,朱海平,罗乾周,杨克俭,王满仓.2007.西昆仑康西瓦北侧蒙古包-普守-带早古生代花岗岩锆石SHRIMP U-Pb测年[J].地质通报,26(6):710-719.
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