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青藏高原东北缘多福屯第三纪钠质基性火山岩及构造启示 被引量:13

Tertiary Duofuton Na-rich mafic volcanic rocks,on northeastern margin of the Qinghai-Tibet Plateau and their tectonic implications
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摘要 位于青藏高原东北缘的多福屯第三纪火山岩,为钠质基性火山岩系。该火山岩(La/Yb)N值在6—11,∑REE平均为117,样品普遍具有不相容元素富集、Pb亏损以及弱的Nb、Ta正异常,Nb/U和Ce/Pb平均值分别为30和17;样品的87^Sr/^86Sr值为0.7041~O.7069,Nd初始值为0.5129(εNd(t)=6),△^207Pb/^240Pb和△^208Pb/^204Pb分别在11~19和73-84之间,结合高的Sr初始值,表现了特征的Dupal(高放射成因铅)异常。地球化学特征表明,该火山岩属于似OIB性质的陆内火山岩,源区具有DM与EMⅡ混合特点。个别岩石表现出明显陆壳混染的迹象。火山岩源区特征反映了OIB类岩石的复杂性,可能由区域原、古特提斯地幔继承而来,因而是原地的和固有的,并非与青藏高原物质向东挤出有关。通过与邻区同时代火山岩的对比推断,整个高原东北缘新生代火山岩幔源区具有小尺度的不均一性。高原东北缘新生代火山岩的发育可能与较大规模的贺兰-川滇南北复合构造有关。 The Tertiary Duofuton volcanic rocks, located on the northeastern margin ol the Qinghai- Tibet Plateau, belong to a Na-rich mafic volcanic system. The rocks are characterized by the(La/Yb)N ratios of 6-11, average EREE of 117, general enrichment in incompatible elements, Pb depletion and weak Nb and Ta positive anomalies. Their Nb/U and Ce/Pb ratios are 30 and 17 on average, respectively. The 87Sr/86 Sr ratios are 0. 704 1-0. 706 9, ^143Nd/^144Nd=0. 512 9(εNa(t)=6), and △^207rpb/^204Pb and △^208Pb/^2044Pb =11-19 and 73-84, respectively. Coupled with high ^87Sr/^86Sr ratios, they show Dupal anomalies. Generally, these marie rocks are OIB-like intracontinental volcanics and the source region exhibits a mixture between DM and EMⅡ , some of the rocks are obviously contaminated by crustal materials. The complexity of OIB for these marie volcanic rocks may have been inherited from the proto- and paleo-Tethyan mantle in the region and hence it is in-situ and original in nature, and possibly not related to the eastward extrusion of materials from the Qinghai-Tibet Plateau. In comparison with coeval volcanics in adjacent areas, it can be inferred that the mantle region in the northeastern margin is heterogeneous on a small scale. The development of the Cenozoic volcanics could have been triggered by the N-S trending tectonics.
出处 《地学前缘》 EI CAS CSCD 北大核心 2007年第3期73-83,共11页 Earth Science Frontiers
基金 国家自然科学基金资助项目(40572138 40234041)
关键词 青藏高原东北缘 多福屯钠质基性火山岩 OIB特征 DM-EMⅡ混合 小尺度不均一地幔 南北复合构造 northeastern margin of the Qinghai-Tibet Plateau Duofuton Na-rich marie volcanics OIB-like mixture of DM-EM Ⅱ small scale heterogeneous mantle S-N trending tectonics
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