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61.
中甸地区甭哥正长岩地球化学特征及其地质意义 总被引:4,自引:0,他引:4
长期以来,甭哥正长岩体被认为是印度—欧亚板块碰撞引起的走滑剪切构造所控制的碱性岩浆活动的产物。本文研究表明甭哥正长岩属钾玄岩系列,富集K2O(5.88%~9.08%)、稀土元素(特别是轻稀土元素)和大离子亲石元素,高场强元素亏损,具有岛弧型微量元素特征。地球化学数据表明原岩于高压条件下发生部分熔融,岩浆源区深度较大,经历了结晶分异作用形成正长岩岩浆。甭哥正长岩的锆石稀释法U-Pb测定年龄为201.4Ma,略晚于中甸弧钙碱性斑岩,其形成的构造环境是弧后拉张环境,甘孜—理塘洋向西低角度俯冲使中甸地区地壳挤压增厚,从而在较深的深度形成原始岩浆。在中甸岛弧岩浆演化后期存在区域性的构造体制转折,从区域性的挤压环境转换成区域性的拉张环境,甭哥岩体的侵位处于两者的过渡时期。 相似文献
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《International Geology Review》2012,54(6):556-582
The Yandangshan syenite is a representative Late Cretaceous igneous pluton cropping out in SE China. U–Pb zircon dating using LA‐ICP‐MS yielded a crystallization age of 98±1 Ma for the syenite. Petrographically and geochemically of shoshonitic affinity, it is enriched in LREE and LILE, and has a pronounced Nb–Ta trough in the primitive mantle‐normalized trace element spider diagram. Zircon ?Hf(t) values vary from ?3.04 to ?7.71, displaying a unimodal distribution. The syenite also has high Sr [(87Sr/86Sr) i = 0.7086–0.7089], low Nd [?Nd(t) = ?6.57 to ?7.64] isotopic ratios, plotting in the enriched mantle field on an ?Nd(t) versus (87Sr/86Sr) i diagram. We propose that the Yandangshan syenite was generated by pyroxene‐dominated high‐pressure fractional crystallization from basaltic magma that was derived from an enriched mantle source. Although coexisting Yandangshan rhyolites have Sr–Nd isotopic compositions similar to the Yandangshan syenite, they were not derived from the same source. Instead, the rhyolitic magma was produced by partial melting of crustal materials as a result of the underplating of basaltic magma. The crust‐like Sr–Nd–Hf isotopic signature of the Yandangshan syenite is ascribed to mantle sources that were enriched by subducted sediments. Formation of Yandangshan syenite may represent roll‐back of the subducting palaeo‐Pacific plate and migration of the arc front to the Yandangshan area at ~98 Ma. 相似文献
67.
豫西磨沟正长岩LA-ICP-MS锆石U-Pb年代学及Hf同位素 总被引:4,自引:0,他引:4
河南省东秦岭地区印支期岩浆活动产物零星出露,豫西外方山纸房—黄庄地区是其产地之一,本文对纸房—黄庄地区出露面积最大的磨沟正长岩岩体进行了LA-ICP-MS锆石U-Pb定年及Hf同位素测试.磨沟正长岩的锆石206 Pb/238U谐和年龄为245.5 ±8.0Ma(95%置信度,MSWD=2.6),记录了秦岭造山带印支期内早三叠世碱性岩浆活动事件.磨沟正长岩样品的εHf(t)值介于-31.89~-10.59之间,聚集于-31.89~-27.64和-21.02~-10.59两个区间内,二阶段Hf模式年龄(tDM2)为1937~3267Ma,集中于1937~ 2591 Ma和3003 ~ 3267 Ma两个年龄范围内.锆石Hf同位素特征表明磨沟正长岩是幔源碱性岩浆与壳源花岗质岩浆(片麻岩部分熔融)相混合的产物,与磨沟正长岩岩体中出现暗色微粒包体这一地质特征相吻合.磨沟正长岩形成于秦岭造山带的面接触碰撞时期,长期持续的碰撞效应使纸房—黄庄岩石圈厚度在垂向上显著增厚,其重力不稳定性加强,在印支早期发生局部小规模拆沉,与之伴有大规模的深部流体活动,暗示纸房—黄庄地区具有巨大成矿潜力,尤其是与正长岩岩体自身相关的稀有(Rb、Zr)、轻稀土元素及非水溶性钾矿资源. 相似文献
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Two petrologically distinct alkali feldspar syenite bodies (AFS-1 and AFS-2) from Chhotaudepur area, Deccan Large Igneous Province are reported in the present work. AFS-1 is characterized by hypidio-morphic texture and consists of feldspar (Or55Ab43 to Or25Ab71), ferro-pargasite/ferro-pargasite horn-blende, hastingsite, pyroxene (Wo47, En5, Fs46), magnetite and biotite. AFS-2 exhibits panidiomorphic texture with euhedral pyroxene (Wo47-50, En22-39, Fs12e31) set in a groundmass matrix of alkali feldspar (Or99Ab0.77 to Or1.33Ab98), titanite and magnetite. In comparison to AFS-1, higher elemental concentra-tions of Ba, Sr and PREE are observed in AFS-2. The average peralkaline index of the alkali feldspar syenites is w1 indicating their alkaline nature. Variation discrimination diagrams involving major and trace elements and their ratios demonstrate that these alkali feldspar syenites have a shoshonite affinity but emplaced in a within-plate and rifting environment. No evidence of crustal contamination is perceptible in the multi-element primitive mantle normalized diagram as well as in terms of trace elemental ratios. The enrichment of incompatible elements in the alkali feldspar syenites suggests the involvement of mantle metasomatism in their genesis. 相似文献
70.
Wang Y.Jiao Y. 《大地构造与成矿学》2015,(1):139-152
The early Jurassic Dashipo-Heishantuo batholith in Beijing, which consists of the Dashipo hornblende-biotite syenite and Heishantuo granite, exposed in the western Yanshan orogenic belt, eastern North China Craton. The Dashipo syenite is magnesian potassic intermediate rock enriched in large ion lithophile elements such as Rb, Ba, Sr, Pb and LREE, and relatively depleted in high field strength elements such as Nb, Ta, U, Th, Zr, Hf as well as P and Ti, with εNd(t) values from -12.1 to -12.2 and ISr values of 0.70506-0.70464. The Heishantuo granite is magnesian peraluminous high K calc-alkaline, with an enrichment of large ion lithophile elements and radioactive elements such as Rb, Ba, Th, U and Pb, and a depletion of HREE and high field strength elements such as Nb, Ta, Zr and Hf as well as Sr, P and Ti, with εNd(t) values from -15.5 to -18.0 and ISr values of 0.70516-0.70593. The magma of the Dashipo syenite is produced by fractional crystallization of mantle-derived K-rich mafic magma under high pressure. The partial melting of the lower crust, which was heated and metasomatised by the mantle-derived magma, produced granitic magma that intruded into the unconsolidated Dashipo syenite to form the concentric batholith. The petrology and geochemistry of the Dashipo hornblende-biotite syenite indicate that the water weakening was important for the lithospheric destruction within the interior part of the North China Craton. Meanwhile, the partial melting related to the double-diffusion of energy and chemical composition between mantle-derived magma and crustal rocks was an important mechanism for the Mesozoic calc-alkaline felsic magmatism occurred in the interior of the North China Craton. ©, 2015, Science Press. All right reserved. 相似文献