SHRIMP Zircon U-Pb Ages, Geochemistry, Nd-Hf-O Isotopic Compositions of the Huai'an Complex in the Northwest of Hebei Province and Its Geological Significance
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摘要: 冀西北地区怀安杂岩由变质表壳岩和变质深成岩组成，其中变质表壳岩的形成时代、怀安杂岩的构造背景以及其与孔兹岩带间的关系一直存在较大争议.本文对怀安杂岩的几处代表性露头进行了详细野外考察，对4件样品进行了岩石学、锆石SHRIMP U-Pb定年、同位素和元素地球化学分析.所有样品都给出了1.86~1.81 Ga的变质锆石年龄，进一步支持怀安杂岩广泛遭受到古元古代晚期变质作用改造的认识.侵入/包裹含BIF表壳岩组合的变质辉长岩（HB1425）和片麻状英云闪长岩（HB1426）分别给出了~2.5 Ga和2.55 Ga的形成年龄，限制表壳岩形成时代老于2.55 Ga，推测为新太古代表壳岩.浅粒岩（HB1431）和紫苏石榴黑云斜长片麻岩（HB1435）中最老的碎屑锆石分别为2.46 Ga和2.51 Ga，可能还存在古元古代的碎屑锆石，表明它们都为古元古代表壳岩.上述结果进一步确定了怀安杂岩中发育两期表壳岩组合.变质辉长岩和片麻状英云闪长岩的全岩εNd（t）、TDM1和TDM2分别为+2.19~+3.06、2.67~2.75 Ga和2.67~2.69 Ga，表明其物源区不存在较大规模的古老陆壳物质，新太古代是怀安地区主要陆壳生长期.变质辉长岩中~1.82 Ga变质锆石中较多具有正的εHf（t）值，最高可达11.1，最可能的解释是古元古代变质过程存在地幔添加作用.锆石的O同位素分析显示区域上可能存在低δ18O的岩石，在古元古代变质过程中，可能存在低δ18O流体对锆石的改造.怀安杂岩和西部孔兹岩带中不同类型岩石的比例明显不同，但两者都同样发育新太古代和古元古代的双层地壳结构，怀安杂岩或许代表孔兹岩带剥蚀更深而出露的深部地壳部分.
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关键词:
- 锆石SHRIMP U-Pb定年 /
- Nd-Hf-O同位素 /
- 怀安杂岩 /
- 表壳岩 /
- 华北克拉通 /
- 地球化学
Abstract: The Huai'an Complex in Northwest Hebei Province consists of meta-supracrustal rocks and metamorphic plutonic rocks. There are still some controversies about some issues such as the formation age of supracrustal rocks, the tectonic setting of Huai'an Complex and the relationship between Huai'an Complex and Khondalite belt. Some representative outcrops of the Huai'an Complex have been studied in detail by field investigation, petrology, zircon SHRIMP U-Pb dating, isotopic and elements geochemistry. All of the 4 samples yielded metamorphic ages of 1.86-1.81 Ga, which further supports the previous view that the Huai'an Complex suffered extensive late Paleoproterozoic metamorphism. The BIF-bearing supracrustal rock assemblage was intruded and enclaved by the meta-gabbro (HB1425) and gneissic tonalite (HB1426), which yielded the formation ages of ca. 2.5 Ga and 2.55 Ga, respectively. It suggests that the supracrustal rocks in this location are older than 2.55 Ga. Leptite (HB1431) and hypersthene garnet biotite plagioclase gneiss (Hy-Grt-Bt-Pl gneiss, HB1435) contain the oldest detrital zircons of 2.46 Ga and 2.51 Ga, respectively, probably together with some Paleoproterozoic zircons, indicating that the supracrustal rocks in the two localities are Paleoproterozoic. These results further confirm the development of two stage supracrustal rock assemblages in the Huai'an Complex. The whole rocks εNd(t), TDM1 and TDM2 of the meta-gabbro and gneissic tonalite are +2.19 to +3.06, 2.67 to 2.75 Ga and 2.67 to 2.69 Ga, respectively, indicating no widespread older continental crust material is involved in their source and the Neoarchean is the main period of continental crust growth in the Huai'an area. Some of the ~1.82 Ga metamorphic zircons in metagabbro yielded positive εHf(t) values up to +11.1. The most likely reason for the Hf isotope composition is the mantle addition during the Paleoproterozoic metamorphic event. The zircon O-isotope shows that there may be rocks with low δ18O in the area, and low δ18O fluid could modify the O-isotope of zircon during the Paleoproterozoic metamorphism. It is concluded that the Huai'an Complex has the similar double-layered crustal structure to the Khondalite Belt although it is different in the proportion of the late Noearchean and Paleoproterozoic rocks. The Huai'an Complex may represent the deeper crustal level of the Khondalite belt due to stronger exhumation.-
Key words:
- zircon U-Pb dating /
- Nd-Hf-O isotopes /
- Huai'an Complex /
- supracrustal rocks /
- North China Craton /
- geochemistry
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图 1 怀安杂岩在华北克拉通的位置（a）及其周边地区早前寒武纪地质简图（b）
图a据Zhao et al.（2005）修改；图b据张家辉等（2019b）修改
Fig. 1. Huai'an Complex of the North China Craton (a) and Precambrain geological sketch of the border area of the Huai'an Complex (b)
图 2 怀安南高崖村BIF铁矿区和变质辉长岩及相关岩石的野外照片和显微照片
a.变质辉长岩（HB1425）；b.片麻状英云闪长岩（HB1426）；c.片麻状英云闪长岩和斜长角闪岩的接触关系；d.斜长角闪岩包体；e.变质辉长岩显微照片；f.片麻状英云闪长岩显微照片.Cpx.单斜辉石；Hbl.普通角闪石；Opx.斜方辉石；Pl.斜长石；Qtz.石英
Fig. 2. Field photos and micrographs of metagabbro and related rocks from Gaoyacun BIF mine in southern of Huai'an
图 3 怀安南大岔口沟和史家庄古元古代晚期孔兹岩系岩石野外照片及显微照片
a.黑云斜长片麻岩遭受深熔作用改造；b.浅粒岩（HB1431）野外特征；c.浅粒岩（HB1431）；d.基性麻粒岩显示深熔作用改造；e.变质碎屑沉积岩；f.变质碎屑沉积岩似保留沉积层理；g.石榴石岩石；h.紫苏石榴黑云斜长片麻岩（HB1435）；i.浅粒岩显微照片；j.紫苏石榴黑云斜长片麻岩显微照片. Bt.黑云母；Grt.石榴子石；Kfs.钾长石；Opx.斜方辉石；Pl.斜长石；Qtz.石英
Fig. 3. Field photos and micrographs of late Paleoproterozoic Khondalite series in Dachakougou and Shijiazhuang, southern of Huai'an
图 4 怀安南高崖村BIF铁矿区的变质辉长岩（HB1425）和片麻状英云闪长岩（HB1426）的锆石阴极发光图像
Fig. 4. Cathodoluminescence (CL) images of zircons from metagabbro (HB1425) and gneissic tonalite (HB1426) in Gaoyacun BIF mine, southern of Huai'an
图 5 怀安南岩石样品的锆石U⁃Pb谐和图
a.变质辉长岩（HB1425）；b.片麻状英云闪长岩（HB1426）；c.变粒岩（HB1431）；d.紫苏石榴黑云斜长片麻岩（HB1435）.
Fig. 5. Concordia diagrams for U⁃Pb data of zircons from the Huai'an Complex in southern of Huai'an
图 6 怀安南怀安杂岩中的古元古代晚期孔兹岩系中变质碎屑沉积岩的锆石阴极发光图像.
a~b.浅粒岩（HB1431）；c~f.紫苏石榴黑云斜长片麻岩（HB1435）
Fig. 6. Cathodoluminescence (CL) images of zircons from meta-clastic sedimentary rocks in the Paleoproterozoic Khondalite series from the Huai'an Complex in southern of Huai'an
图 7 怀安南怀安杂岩中岩石样品的锆石O同位素组成
图中给出了未受后期影响的太古亩岩浆锆石δ18O值变化范围（点线长方形区域据Valley et al., 2005）
Fig. 7. O-in-zircon isotopic compositions for rocks from the Huai'an Complex in southern of Huai'an
图 8 怀安南怀安杂岩中变质辉长岩（HB1425）的锆石Hf同位素组成
图中红色实线为亏损地幔εHf(t)演化线，两条绿色虚线分别为2.5 Ga和3.0 Ga地壳的εHf(t)的演化线，平均地壳的176Lu/177Hf采用（Griffin et al., 2002）推荐的值（0.015）
Fig. 8. Hf-in-zircon isotopic composition for metagabbro (HB1425) from the Huai'an Complex in southern of Huai'an
图 9 怀安南怀安杂岩中岩石样品的球粒陨石标准化REE模式（a）和MORB标准化微量元素蛛网图（b）
标准化数据来自Sun and McDonough (1989)和Pearce (1983)
Fig. 9. Chondrite-normalized REE patterns (a) and MORB-normalized trace element spider diagrams (b) of samples from the Huai'an Complex
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