Records of the Late Jurassic Magmatic Arc in Heihe Area, Heilongjiang Province: Discussion on the Relationship with Mongolia-Okhotsk Ocean
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摘要: 黑龙江黑河北部的黑花山地区广泛发育中生代的侵入岩，但该侵入岩的形成时代、岩石组合、成因仍然不清.对黑花山地区侵入岩进行了野外、岩相学、岩石学、年代学、岩石地球化学等研究，以探讨该套岩石形成的时代、原因及大地构造背景.对两件二长花岗岩开展的LA-ICP-MS锆石U-Pb测年获得加权平均年龄分别为148.7±0.6 Ma、153.50±0.56 Ma，表明其形成于晚侏罗世.岩石组合主要为含有少量英云闪长岩（T1）、奥长花岗岩（T2）的T1T2G（狭义花岗岩）组合，即弧环境的侵入岩组合.上述岩石组合富硅、碱、高钾、过铝（A/CNK大于1）、低Fe2O3T.其在SiO2-K2O图上为高钾钙碱系列，硅镁图中为低铁钙碱（LF-LA）系列，Peacock指数为钙碱性或碱钙性，痕量元素蛛网图显示富集大离子亲石元素，亏损Nb、Ta、P、Ti、Y、Yb等元素.稀土元素配分模式为右倾型，轻稀土相对富集，（La/Yb）n=13.78~29.85，无负Eu异常或弱正Eu异常或弱的Eu负异常.花岗岩类具有高Sr低Y的特征，Sr/Y比值介于29.53~103.80，具有“C型”埃达克岩的特征.上述岩石组合及其特征均指示了弧火成岩的性质，结合构造环境判别认为该区晚侏罗世花岗岩类形成于蒙古-鄂霍茨克洋的南向俯冲有关的环境，岩浆可能源于兴安弧加厚下地壳的部分熔融作用.Abstract: The Mesozoic intrusive rocks are widely developed in Heihuashan area in the north of Heihe City, Heilongjiang Province, but the formation age, rock assemble age and genesis of the intrusive rocks are still unclear. In this paper, the intrusive rocks in Heihuashan area have been studied in the field, petrography, petrology, geochronology and petrochemistry, in order to discuss the formation age, petrogenesis and geotectonic background of these rocks, For two monzonitic granites, the weighted average ages of zircon U-Pb dating by LA-ICP-MS are 148.7±0.6 Ma and 153.50±0.56 Ma respectively, indicating that they were formed in the Late Jurassic. The intrusive rock assemblage of tonalite(T1), trondhjemite(T2), and granite(G) etc indicates a rock assembleage of T1T2G in arc environment. The above granitoids are rich in silicon, alkali, high potassium, peraluminium (A/CNK is greater than 1), and low in Fe2O3T. The rocks belong to high potassium calcium alkali series in the SiO2-K2O diagram, low Fe- calcium alkali (LF-CA) series in SiO2-MgO diagram and calcium alkali or alkali calcium in SiO2-(Na2O+K2O-CaO)diagram. The distribution pattern of rare earth element is right-leaning, with LREE relatively enriched and HREE depleted, giving (La/Yb)n=13.78-29.85 and no negative Eu anomaly or weak positive Eu anomaly or weak negative Eu anomaly.The granitoids are characterized by high Sr and low Y, with Sr/Y ratio ranging from 29.53 to 103.80, which are characteristic of "C-type" adakites. The above rock assemblages and their characteristics all indicate the properties of arc igneous rocks. Combined with the tectonic environment, it is believed that the Late Jurassic granitoids in this area were formed in the southwardly subduction environment of the Mongolia-Okhotsk Ocean.The magma maybe derived from the partial melting of the thickening lower crust of Xing'an Arc.
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Key words:
- Heihuashan area /
- Heihe, Heilongjiang Province /
- granitoids /
- geochemistry /
- Late Jurassic /
- magmatic arc
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图 1 大地构造位置简图(a)和黑花山地区区域地质简图(b)
1.古元古界兴华渡口岩群黑云斜长片麻岩; 2.新元古界落马湖岩群北宽河组大理岩; 3.新元古界落马湖岩群嘎拉山岩组黑云石英片岩; 4.晚侏罗世二长花岗岩; 5.早侏罗世花岗闪长岩; 6.白垩系龙江组安山岩; 7.早白垩世二长花岗岩; 8.早白垩世花岗闪长岩; 9.龙江期辉长岩脉; 10.早白垩世石英正长斑岩脉; 11.第四系; 12.本文采样点; 13.钼矿; 14.研究区15.收集前人的采样点；根据赵焕利和李仰春（2009)修改
Fig. 1. Geotectonic location sketch map and regional geological map of the study area
图 2 黑花山地区花岗岩类野外与显微照片
a.含钾长石巨斑花岗岩；b.似斑状花岗岩；c.似斑状二长花岗岩单偏光显微镜下；d.似斑状二长花岗岩正交偏光显微镜下；e.二长花岗岩单偏光显微镜下；d.二长花岗岩正交偏光显微镜下；g.二长花岗岩单偏光显微镜下；h.二长花岗岩正交偏光显微镜下；Pl.斜长石；Kf.钾长石；Bt.黑云母；Q.石英
Fig. 2. Field photos and microscopic photos of the granitoids in Heihuashan area
图 3 SJY20160813-1样品锆石阴极发光图像（单位：Ma）
Fig. 3. Cathodoluminescence images of zircon from sample SJY20160813-1
图 4 SJY20160813-6样品锆石阴极发光图像（单位：Ma）
Fig. 4. Cathodoluminescence images of zircon from sample SJY20160813-6
图 5 黑花山地区花岗岩的LA-ICP-MS锆石U-Pb年龄谐和图
Fig. 5. Zircon LA-ICP-MS U-Pb concordia diagrams of the granitoids in Heihuashan area
图 6 TAS图解（a）及TTG类判别图解（b）
a.据Eric（1994），图中虚线为碱性和亚碱性分界线, 据Irvine and Baragar（1971）; b.据O’Connor（1965）
Fig. 6. TAS diagram(a)and TTG type discrimination diagram of granite(b)
图 10 黑花山地区侵入岩痕量元素原始地幔标准化蛛网图（a）和稀土元素球粒陨石标准化配分模式图（b）（标准化值据Sun and McDonough, 1989）
Fig. 10. Primitive mantle normalized trace element spider diagrams(a) and chondrite-normalized REE patterns(b) of granitic rocks in Heihuashan area(modified from Sun and McDonough, 1989)
图 11 黑花山地区侵入岩的Sr/Y-Y图
Fig. 11. Diagram of Sr/Y-Y of intrusive rocks in Heihuashan area
图 12 SiO2-MgO图
HT-HMA.高温-高镁安山岩; MT-HMA.中温-高镁安山岩; LT-HMA.低温-高镁安山岩; 据邓晋福（2010）
Fig. 12. SiO2-MgO diagram
图 13 构造环境判别图
VAG.火山弧花岗岩；WPG.板内花岗岩；syn-COLG.同碰撞花岗岩；ORG.洋中脊玄武岩；据Pearce et al.（1984）
Fig. 13. Discrimination diagrams of tectonic setting
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