新疆东准噶尔绿石沟高Ba-Sr石英二长岩的锆石U-Pb年龄、成因及地质意义
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摘要
绿石沟岩体位于东准噶尔琼河坝矿集区,向东侵入到绿石沟铜矿赋矿围岩中泥盆统北塔山组火山岩中。LA-ICP-MS锆石U-Pb测年显示该岩体形成于354±1Ma,为早石炭世。其主要岩石类型为石英二长岩,含有大量的基性微粒包体,具有较高的硅、钙、钾含量(SiO_2=62.31%~65.31%,CaO=3.71%~4.89%,K_2O=2.85%~3.54%),属高钾钙碱性系列。铝含量较高(Al_2O_3=15.44%~16.29%),属准铝质(A/CNK=0.93~0.99,A/NK=1.68~1.96)Ⅰ型花岗岩。稀土元素总量较低(ΣREE=90.82×10~(-6)~111.36×10~(-6)),轻稀土元素相对富集,Eu呈弱的负异常(δEu=0.68~0.87)。富集大离子亲石元素(K、Rb、Ba、Sr等),亏损高场强元素(Nb、Ta、P、Ti等),具有高Ba(758×10~(-6)~1113×10~(-6))、Sr(401.8×10~(-6)~512.5×10~(-6))含量和高的(La/Yb)_N、Sr/Y值,显示出高Ba-Sr花岗岩的特征,应是幔源基性岩浆与壳源岩浆混合的产物,可能形成于俯冲环境向造山后环境的构造转换阶段。
The Liishigou pluton is located in the Qiongheba ore concentration area in East Junggar. This pluton intruded into the host rock of the Lushigou copper deposit. LA-ICP-MS U-Pb dating of zircons from this pluton yielded an early Carboniferous age of 354 ± 1 Ma. The main rock type of the pluton is quartz-monzonite with many mafic-ultral mafic enclaves inside. These quartz-monzonites have high SiO_2(62.31%~65.31%), Al_2O_3(15.44%~16.29%),CaO(3.71%~4.89%) and K_2O(2.85%~3.54%) contents,exhibiting high-K calcalkaline and metaluminous characteristics(A/CNK=0.93~0.99,A/NK=1.68~1.96),and belonging to I-type granite. The total REE values of them are low(90.82×10~(-6)~111.36×10~(-6)) with relative enrichment of LREE and Eu negative anomaly(δEu=0.68~0.87). The primitive mantle normalized trace element patterns are characterized by the enrichment of the LILE(K, Rb, Ba, Sr) and depletion of the HFSE(Nb, Ta, P, Ti). The quartz-monzonite has high Ba(758×10~(-6)~1113×10~(-6)),Sr(401.8×10~(-6)~512.5×10~(-6)) values with high(La/Yb)_N, Sr/Y ratios, distinct Nb, Ta and Ti depletion, and are comprehensively called high Ba-Sr granitoid.These characters indicate that the Liishigou pluton was probably formed by the magma-mixing of the mantle-derived mafic magma and crustal partial melting magma during the tectonic transition period from subduction to post-orogenic setting in the late Paleozoic.
The Liishigou pluton is located in the Qiongheba ore concentration area in East Junggar. This pluton intruded into the host rock of the Lushigou copper deposit. LA-ICP-MS U-Pb dating of zircons from this pluton yielded an early Carboniferous age of 354 ± 1 Ma. The main rock type of the pluton is quartz-monzonite with many mafic-ultral mafic enclaves inside. These quartz-monzonites have high SiO_2(62.31%~65.31%), Al_2O_3(15.44%~16.29%),CaO(3.71%~4.89%) and K_2O(2.85%~3.54%) contents,exhibiting high-K calcalkaline and metaluminous characteristics(A/CNK=0.93~0.99,A/NK=1.68~1.96),and belonging to I-type granite. The total REE values of them are low(90.82×10~(-6)~111.36×10~(-6)) with relative enrichment of LREE and Eu negative anomaly(δEu=0.68~0.87). The primitive mantle normalized trace element patterns are characterized by the enrichment of the LILE(K, Rb, Ba, Sr) and depletion of the HFSE(Nb, Ta, P, Ti). The quartz-monzonite has high Ba(758×10~(-6)~1113×10~(-6)),Sr(401.8×10~(-6)~512.5×10~(-6)) values with high(La/Yb)_N, Sr/Y ratios, distinct Nb, Ta and Ti depletion, and are comprehensively called high Ba-Sr granitoid.These characters indicate that the Liishigou pluton was probably formed by the magma-mixing of the mantle-derived mafic magma and crustal partial melting magma during the tectonic transition period from subduction to post-orogenic setting in the late Paleozoic.
引文
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