赣中山庄二长花岗岩的成因与构造背景:岩石学、地球化学及锆石U-Pb年代学证据
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摘要
赣中山庄花岗岩岩体位于钦杭成矿带的南侧,岩性上包括二长花岗岩和花岗闪长岩。本文对岩体北部的二长花岗岩开展了年代学、地球化学及同位素研究以约束该岩体的形成时代、岩石成因及成岩构造背景。锆石CL图像、Th/U比值,以及(Sm/La)_N-La和Ce/Ce~*-(Sm/La)_N图解均表明,二长花岗岩所有锆石晶体为岩浆成因;其中第一组锆石加权平均年龄为420～419Ma,代表了岩浆结晶年龄。该花岗岩SiO_2含量为71.48%～66.20%、K_2O/Na_2O值为1.24～0.99、A/CNK>1.1;结合白云母和石榴石的出现、ACF图解、Rb-Th、Rb-Y的负相关性,山庄二长花岗岩属高钾钙碱性强过铝质S型花岗岩。同时,该岩石亏损大离子亲石元素Ba和Sr以及高场强元素Nb和Ta,说明系壳源物质部分熔融的产物。CaO/Na_2O值(0.14～0.07)、Rb/Sr值(8.27～3.83)、Rb/Ba值(1.48～0.82)、FeO~T+MgO+TiO_2含量(2.4～1.8)和二阶段Nd模式年龄(t_(2DM)=2031～1971Ma)进一步说明二长花岗岩的源岩是古元古代的富粘土的泥质岩。锆石的饱和温度和Ti温度计计算结果表明二长花岗岩岩浆形成温度为722～720℃,黑云母的全铝温度计则反映其形成压力为3.21～2.71kbar。结合花岗岩构造环境判别图以及华南大地构造演化特征,山庄花岗岩岩体可能是在后碰撞环境下由古元古代富粘土泥质岩于低温低压条件下部分融熔的结果。
This paper presents a systemic study on geochronology,geochemistry and Sr-Nd isotopes of the northern monzogranite from Shanzhuang granitic pluton located on the southern part of the Qinhang Metallogenic Belt in central Jiangxi Province which comprises monzogranite and granodiorite to constrain its emplacement age,petrogenesis and tectonic setting. All zircons from the monzogranite are confirmed to be of magmatic origin by CL imaging,Th/U ratio and diagrams of( Sm/La)_N-La and Ce/Ce~*-( Sm/La)_N and are divided into three groups. The weighted mean age( 420 ～ 419 Ma) of the first group is interpreted as crystallization age of the monzogranite. The Shanzhuang monzogranite,which has SiO_2 content of 71. 48% ～ 66. 20%,K_2O/Na_2O ratio of 1. 24 ～ 0. 99 and A/CNK ratio of > 1. 1,with the emergences of muscovite and garnet as well as ACF diagram and negative correlations of Rb with Th and Y,belongs to high K calc-alkaline,strongly peraluminous S-type granite. Meanwhile,this type rock defined by a depletion in large ion lithophile elements Ba and Sr and high field strength elements Nb and Ta is interpreted as a product of partial melting of the crustderived materials. The ratios of CaO/Na_2O( 0. 14 ～ 0. 07),Rb/Sr( 8. 27 ～ 3. 83) and Rb/Ba( 1. 48 ～ 0. 82),the content of FeO~T+MgO + TiO_2( 2. 4 ～ 1. 8) and the t_(2DM) ages( 2031 ～ 1971 Ma) together suggest that the protolith of the monzogranite is Paleoproterozoic clay-rich argillaceous rocks. Moreover,the monzogranite is likely formed at a temperature condition( 722 ～ 720℃) constrained by saturation-and Ti temperatures of zircon,and a pressure condition of 2. 71 ～ 3. 21 kbar constrained by the Ti-in-biotite geothermometer.Combined with the Paleozoic tectonic development of South China,the diagram of Rb-( Y + Nb) shows that the geological setting of Shanzhuang granitic pluton is post-collision. In summary,the Shanzhuang pluton was formed by partial melting of Paleoproterozoic clayrich argillaceous rocks at a low temperature and a low pressure condition under post-collisional setting.
This paper presents a systemic study on geochronology,geochemistry and Sr-Nd isotopes of the northern monzogranite from Shanzhuang granitic pluton located on the southern part of the Qinhang Metallogenic Belt in central Jiangxi Province which comprises monzogranite and granodiorite to constrain its emplacement age,petrogenesis and tectonic setting. All zircons from the monzogranite are confirmed to be of magmatic origin by CL imaging,Th/U ratio and diagrams of( Sm/La)_N-La and Ce/Ce~*-( Sm/La)_N and are divided into three groups. The weighted mean age( 420 ～ 419 Ma) of the first group is interpreted as crystallization age of the monzogranite. The Shanzhuang monzogranite,which has SiO_2 content of 71. 48% ～ 66. 20%,K_2O/Na_2O ratio of 1. 24 ～ 0. 99 and A/CNK ratio of > 1. 1,with the emergences of muscovite and garnet as well as ACF diagram and negative correlations of Rb with Th and Y,belongs to high K calc-alkaline,strongly peraluminous S-type granite. Meanwhile,this type rock defined by a depletion in large ion lithophile elements Ba and Sr and high field strength elements Nb and Ta is interpreted as a product of partial melting of the crustderived materials. The ratios of CaO/Na_2O( 0. 14 ～ 0. 07),Rb/Sr( 8. 27 ～ 3. 83) and Rb/Ba( 1. 48 ～ 0. 82),the content of FeO~T+MgO + TiO_2( 2. 4 ～ 1. 8) and the t_(2DM) ages( 2031 ～ 1971 Ma) together suggest that the protolith of the monzogranite is Paleoproterozoic clay-rich argillaceous rocks. Moreover,the monzogranite is likely formed at a temperature condition( 722 ～ 720℃) constrained by saturation-and Ti temperatures of zircon,and a pressure condition of 2. 71 ～ 3. 21 kbar constrained by the Ti-in-biotite geothermometer.Combined with the Paleozoic tectonic development of South China,the diagram of Rb-( Y + Nb) shows that the geological setting of Shanzhuang granitic pluton is post-collision. In summary,the Shanzhuang pluton was formed by partial melting of Paleoproterozoic clayrich argillaceous rocks at a low temperature and a low pressure condition under post-collisional setting.
引文
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