Geochemistry, zircon chronology, Sr-Nd-Hf isotopic characteristics and subduction magmatism of Heishidun basic rocks in the East Tianshan
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摘要:
在东天山康古尔塔格南黑石墩一带新发现一套基性岩，岩性以辉长岩和橄榄辉长岩为主，岩石具有相对较低SiO2（47.59%~50.79%）、富Na2O（2.72%~4.42%）贫K2O（0.26%~1.15%），低MgO（3.94%~12.55%），中等Mg#（47.6~66.64），高Al2O3（14.75%~19.65%），相对富集轻稀土（（La/Yb）N1.83~2.12），Eu弱正异常（1.00~1.25），富集LILE（Ba、U、Sr），亏损HFS（Ta、Nb、Th和Ti），并强烈富集Pb。锆石LA-ICP-MS U-Pb年龄（（342.6±3.2）Ma）表明该基性岩属于早石炭世岩浆活动的产物。岩石具有较低的（87Sr/86Sr）i（0.703421~0.704551），正的εNd（t）（7.6~8.1）和εHf（t）（9.82~13.74）。地球化学特征和岩相学显示其来自亏损的岩石圈地幔源区，且源区在较低程度的部分熔融前受到俯冲板片中富含大离子亲石和轻稀土元素的海洋沉积物在俯冲过程中脱水熔融形成流体的交代作用影响，原始岩浆在侵位过程中发生程度不同的橄榄石、辉石和斜长石分离结晶作用，侵位过程中受到地壳物质混染的程度非常低。构造和动力学背景研究表明，黑石墩基性岩为北天山洋在早石炭世沿康古尔塔格—黄山大断裂向北俯冲阶段的产物。
Abstract:A new set of basic rocks was discovered in the Heishidun in South Kangurtag, Eastern Tianshan. Its lithology mainly consists of gabbro and olive gabbro. The rocks are characterized by relatively low contents of SiO2 (47.59%-50.79%), K2O (0.26%-1.15%) and MgO (3.94%-12.55%), high contents of Na2O (2.72% -4.42%) and Al2O3 (14.75% -19.65%), and moderate content of Mg# (47.6-66.64). Light rare earth is enriched ((La/Yb)N of 1.83-2.12) with a bit of Eu positive anomaly (1.00-1.25). LILE (Ba, U, Sr) is enriched, while HFS (Ta, Nb, Th, and Ti) is depleted, and Pb is strongly enriched. LA-ICP-MS zircon U-Pb dating yields 342.6±3.2 Ma, indicating that this basic rock is a product of Early Carboniferous magmatic activity. Rocks have lower Sr ratio (87Sr/86Sr)i (0.703421-0.704551), positive εNd (t) (7.6-8.1) and εHf (t) (9.82-13.74). Geochemical characteristics and petrography show that it is originated from the lithospheric mantle source of the loss, and the source area was affected by the metamorphism of the dehydration and melting fluids resulted from the subduction of marine sediments rich in large ionic lithophile and light rare earth elements. The separation and crystallization of olivine, pyroxene and plagioclase took place during the emplacement of magma, the degree of contamination by the crustal material during the emplacement was very low. The structural and dynamic background shows that the Heishidun basic rock is the product of the Northern Tianshan Ocean's northward subduction along the Kangugtag-Huangshan fault in the Early Carboniferous.
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图 5 黑石墩基性岩稀土元素球粒陨石标准化配分曲线（a）和微量元素原始地幔标准化蛛网图（b）(据Sun and McDonough, 1989)
Figure 5.
图 10 主量及微量元素构造环境判别图解(a, 据Meschede, 1986;b, 据Pearce and Cann, 1973;c, 据Mullen, 1983;d, 据Wood et al., 1979)
Figure 10.
表 1 黑石墩基性岩岩石地球化学数据（含量单位: 主量元素为%, 微量元素为10-6）
Table 1. Major elements (%) and trace elements(10-6)data of the Heishidun basic rocks
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表 2 黑石墩辉长岩LA-ICP-MS锆石U-Pb同位素数据
Table 2. LA-ICP-MS zircon U-Pb dating results of Heishidun gabbro
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表 4 黑石墩基性岩的全岩Sr-Nd同位素组成
Table 4. Whole-rock Sr-Nd isotopic compositions of Heishidun basic rocks
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