Petrogenesis of the late Mesozoic Lingshang ultramafic intrusion in northern Jiangxi Province:Chronologic and geochemical constraints
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摘要:
华南内陆在晚中生代发生了广泛的岩石圈伸展减薄事件，赣北新余地区的岭上超镁铁岩体形成于（120.8±1.4）Ma的早白垩世晚期，其作为钦杭结合带东段早白垩世幔源岩浆活动的记录，是研究华南中部晚中生代地幔属性及地球深部动力学过程的良好对象。在系统分析岭上超镁铁质岩的LA-MC-ICP-MS锆石U-Pb年代学、Lu-Hf同位素和元素地球化学特征的基础上，探讨了该超镁铁质岩的源区特征及其所反映的大地构造背景。数据表明，岭上超镁铁岩在形成过程中未遭受明显的地壳混染，其MgO含量集中且与TiO2、Al2O3、Ni、Th等元素之间不存在明显的线性关系，反映该岩体未发生显著的结晶分异作用。但Mg#的变化范围和La-Sm分异程度反映堆晶作用和部分熔融可能对岩浆演化有所影响。稀土和微量元素（如Nb、Ta、Zr、Hf等）特征类似于板内玄武岩（OIB），低SiO2、高Ti、高Fe/Mn比值和Ni等特征均显示与软流圈地幔关系密切。但锆石εHf（t）（6.83~11.41）未达到亏损地幔的程度、Nb/Ta比值接近于岩石圈地幔值，且在相关元素图解中具尖晶石橄榄岩地幔源区低程度部分熔融的特征。反映岭上超镁铁岩可能是晚中生代陆内伸展背景下，上涌的软流圈物质与富集岩石圈地幔相互作用并发生部分熔融，深部超镁铁质岩浆沿构造薄弱带快速侵位的产物。
Abstract:Extensive lithospheric extensional thinning events occurred during the late Mesozoic in the interior of South China block. As a record of the early Cretaceous ((120.8±1.4)Ma) mantle-derived magmatic activities in the eastern part of the Qingzhou-Hangzhou juncture belt, the Lingshang ultramafic intrusion in Xinyu of northern Jiangxi is a good object for studying the mantle attribute and geodynamic process of the late Mesozoic in central South China. Based on a systematic analysis of the geochronology from La-MC-ICP-MS zircon U-Pb, Lu -hf isotopes and element geochemistry of the Lingshang ultramafic rocks, the authors investigated the intrusion, the source area characteristics of the ultramafic intrusion and the tectonic background reflected by them. Lingshang ultramafic intrusion suffered no significant crustal contamination. The content of MgO is concentrated with no obvious linear relationship with TiO2, Al2O3, Ni, Th, and some other components, implying no significant crystallization differentiation. However, the range of Mg# and La-Sm differentiation indicates that heap crystallization and partial melting might have exerted an effect on magmatic evolution. The characteristics of rare earth and trace elements (Nb, Ta, Zr, Hf, etc.) are similar to those of intraplate basalt (OIB), and the characteristics of low SiO2, high Ti, high Fe/Mn ratio and Ni are all closely related to asthenosphere mantle. However, the εHf(t) of zircons (6.83-11.41) are less than the value of the depleted mantle, and Nb/Ta ratios are close to the ratio of lithospheric mantle, suggesting low degree partial melting of spinel peridotite mantle source region in the relevant element diagram. All of these data suggest that the Lingshang ultramafic intrusion may be the result of the interaction between asthenosphere mantle and lithospheric mantle under the background of late Mesozoic intracontinental extension. The upwelling asthenosphere material led to the low-degree partial melting of the preexisting spinel peridotite mantle source area, and the deep ultramafic magma was emplaced rapidly along the tectonic weak zone to form the Lingshang ultramafic intrusion.
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图 1 钦杭结合带东段地质简图(a)和岭上超镁铁岩体地质简图(b)
1—钦杭结合带；2—前寒武基底；3—超镁铁岩；4—晚中生代基性岩/A型花岗岩/伸展构造；5—南雄组；6—安源组；7—佘田桥组；8—神山组YJF—宜丰—景德镇断裂；PGJSF—萍乡—广丰—江山—绍兴断裂
Figure 1. Geological schematic map of Qinzhou-Hangzhou juncture belt (a) and Lingshang ultramafic intrusion (b)
1-Qinzhou-Hangzhou junction belt; 2-Precambrian basement; 3-Ultramafic; 4-Late Mesozoic basic rock/A-type granite/extensional structure; 5- Nanxiong Formation; 6-Anyuan Formation; 7-Shetianqiao Formation; 8-Shenshan Formation YJF-Yifeng-Jingdezhen Fault; PGJSF-Pingxiang-Guangfeng-Jiangshan-Shaoxing Fault
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图 2 岭上超镁铁岩野外和显微照片
a—岭上超镁铁岩露头特征；b—岭上超镁铁岩手标本特征；c, d—岭上超镁铁岩显微特征
Figure 2. Field photographs and Microscopic photographs of ultramafic rocks from Lingshang ultramafic intrusion
a − Outcrop characteristic of Lingshang ultramafic rock; b − Hand specimens characteristics of Lingshang ultramafic rock; c, d − Microscopic characteristics of Lingshang ultramafic rocks
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图 3 锆石U−Pb年龄谐和图(a)、锆石εHf(t)图解(b)、锆石阴极发光特征(c)
Figure 3. The zircon U − Pb concordia diagrams (a), probabilistic histogram of age distributions of zircons and εHf(t) versus (b), the character of CL images for zircon (c)
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图 4 岭上岩体超镁铁岩Al2O3−MgO−CaO图解(a, 据Coleman, 1977)和SiO2−Fe2O3T/MgO图解（b）
MP—地幔岩; UC—超镁铁堆晶岩; MC—镁铁堆晶岩
Figure 4. Diagram of Al2O3−MgO−CaO from Lingshang ultramafic intrusion (a, after Coleman, 1977) and SiO2−Fe2O3T/MgO
Mp−Rocks from mantle; UC−Ultramafic cumulate; MC−Mafic cumulate
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图 5 岭上超镁铁岩体的稀土元素配分曲线(a)和微量元素蛛网图(b)
Figure 5. Chondrite-normalized rare earth element (REE) patterns (a) and primitive-mantle-normalized multi-element diagrams(b) of Lingshang ultramafic intrusion
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图 6 岭上超镁铁岩Th/Yb-Ta/Yb图解(a) (据Pearce et al., 1995)和(La/Nb)PM- (Th/Ta)PM图解(b)(据Neal et al., 2002)
TH—拉斑玄武岩; CA—钙碱性玄武岩; NMORB—正常洋中脊型玄武岩; EMORB—富集洋中脊型玄武岩; OIB—洋岛玄武岩; 矢量箭头分别表示俯冲组分(S)，板内富集(W)，结晶分异(F)和地壳混染(C)的影响
Figure 6. Diagram of Ta/Yb versus Th/Yb (a) (after Pearce et al., 1995) and (La/Nb)PM versus (Th/Ta)PM (b) (after Neal et al., 2002).
TH-Tholeiite; CAB-Calc-alkaline basalt; NMORB-Normal mid-ocean ridge basalt; EMORB-Enrichment mid-ocean ridge basalt; OIB-Ocean island basalt; The vector arrows show the effects of subduction components (S), intraplate enrichment (W), crystal differentiation (F), and crustal mixing (C), respectively
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图 7 La-La/Sm图解(a), Ta/La-Hf/Sm图解(b), Sm/Yb-La/Sm图解(c)和Zr/Nb-Ce/Y图解(d)(据Hardarson et al., 1991)
OIB—洋岛玄武岩；NMORB—正常洋中脊型玄武岩；CLM—大陆岩石圈地幔；PM—原始地幔；DM—亏损地幔
Figure 7. Diagram of La-La/Sm(a), Ta/La-Hf/Sm(b), Sm/Yb-La/Sm(c) and Zr/Nb-Ce/Y(d) (after Hardarson et al., 1991)
OIB-Oceanic island basalt; NMORB-Normal mid-ocean ridge basalt; CLM-Continental lithospheric mantle; PM-Primitive mantle; DM-Depleted mantle
表 1 岭上超镁铁岩锆石U−Th−Pb同位素分析结果
Table 1 Analytical results of U−Th−Pb isotopes for intrusion of Lingshang
下载: 导出CSV
表 3 岭上超镁铁岩体的主量(%)和微量(10-6)元素
Table 3 Major (%) and trace element (10-6) compositions of Lingshang ultramafic intrusion
下载: 导出CSV
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