Age, geochemical features and possible petrogenesis mechanism of Early Permian magnesian diorite in Hatu, Xinjiang
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摘要:
西准噶尔别鲁阿嘎希地区广泛发育富镁闪长质小岩体和岩墙。对岩墙全岩样品的Ar-Ar测年获得了292±3Ma的坪年龄，显示其主要形成于早二叠世。这些小岩体和岩墙均为钙碱性系列岩石，具有宽的SiO2(51.9%~62.6%)、高的MgO (Mg#>60)、Cr (45.8×10-6~539×10-6)、Ni (17.2×10-6~197×10-6) 含量，富集大离子亲石元素 (LILE)(如K、Rb、Ba、Th和U)、亏损高强场元素 (如Nb、Ta、Ti)，富集LREE，亏损HREE。这些特征类似于日本中新世Setouchi火山岩带中的赞岐岩。这些岩体/岩墙很可能是在俯冲过程中，经洋壳板片的脱水形成流体与地幔橄榄岩相互作用而成。这表明，西准噶尔别鲁阿嘎希地区早二叠世为岛弧环境。而富镁闪长岩的形成过程也有利于铜-金矿床的形成，显示该区有良好的成矿远景。
Abstract:Magnesian dioritic dikes and plutons widely occur in the Bieluagaxi region, Western Junggar and recorded the Late Paleozoic tectonic evolutionary history of the area.Ar-Ar dating on rock chips of the dikes has yielded a plateau age of 292Ma, indicating an Early Permian age for the dikes.The magnesian diorites are calc-alkaline suite with variable SiO2(51.9%~62.6%), and characterized by high Mg (Mg#>60), Cr (45.8×10-6~539×10-6), Ni (17.2×10-6~197×10-6) contents.The magnesian diorites are strongly enriched in large-ion-lithophile elements (such as K, Rb, Ba, Th and U) and light rare earth elements, and are characterized by depletion of high-field-strength elements (such as Nb, Ta, Ti) and heavy rare earth element.These geochemical features are analogous to those of sanukitoids in Setouchi volcanic belt.The Bieluagaxi magnesian diorite is generated by interaction of mantle peridotite with supercritical fluid derived from dehydration of subducting oceanic slab.The occurrence of Early Permian sanukitic rocks in the Bieluagaxi region suggest that the Western Junggar was dominated by subduction-related environment.The interaction between high oxygen fugacity supercritical fluid and mantle peridotite caused the decomposition of metal sulfides and the Cu and Au mineralization which have good metallogenic prospects in the Bieluagaxi region.
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Key words:
- Magnesian diorite /
- Dikes /
- Subduction zones /
- Cu-Au mineralization /
- Western Junggar
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图 1
西准噶尔地区地质简图据(安芳和朱永峰，2007修改)
Figure 1.
Simplified geological map of the western Junggar region (modified after An and Zhu, 2007)
图 2
别鲁阿嘎希地区地质略图 (据金成伟和徐永生，1997修改)
Figure 2.
Simplified geological map of the Bieluagaxi region (after Jin and Xu, 1997)
图 3
别鲁阿嘎希地区岩墙全岩40Ar/39Ar坪年龄及等时线年龄图
Figure 3.
40Ar/39Ar plateau and isochronal ages for whole rock in the Bieluagaxi region
图 5
别鲁阿嘎希地区岩石的SiO2-MgO图解 (据McCarro and Smellie, 1998)
Figure 5.
SiO2 vs.MgO diagram of rocks from the Bieluagaxi region (after McCarro and Smellie, 1998)
图 6
别鲁阿嘎希地区岩石的球粒陨石标准化REE分布模式图 (球粒陨石标准化值据Sun and McDonough, 1989)
Figure 6.
Chondrite-normalized REE patterns for rocks in the Bieluagaxi region (normalization values after Sun and McDonough, 1989)
图 7
别鲁阿嘎希地区的岩石微量元素原始地幔标准化蛛网图 (原始地幔值据Sun and McDonough, 1989)
Figure 7.
Primitive mantle-normalized spidergram of trace elements for rocks in the Bieluagaxi region (normalization values after Sun and McDonough, 1989)
图 8
别鲁阿嘎希地区的岩石sanukite、adakite、boninite和bajaite判别图 (据Kamei et al., 2004)
Figure 8.
Discrimination diagrams for sanukite, adakite, boninite and bajaite from rocks in the Bieluagaxi region (after Kamei et al., 2004)
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