Abstract:

In order to determine the genesis of the hornblendite enclaves in the Jinling magmatic complex of intrusions in the Western Shandong Province, petrological, mineralogical and geochemical analyses have been conducted on the hornblendites from the complex. The hornblendites show clearly cumulus structure and are composed of plagioclases and amphiboles. The amphiboles in hornblendite enclaves can be divided into two types. The first type of amphibole shows lower SiO₂ but higher Al₂O₃ contents and is classified as the pargasite with magmatic genesis. The other type of amphibole is composed of actinolite, magnesiohornblende and edenite with higher SiO₂ but lower Al₂O₃, which may be attributed to modifications of the magmatic amphiboles during later tectonothermal events. The crystallization pressure of hornblendite enclaves is estimated to be 0.48 GPa using the hornblende Al₂O₃ geobarometer. The hornblendite enclaves show similar characters of the REE and trace elements to those of the hosting dioritic rocks, and are characterized by the LREE enrichment but HREE depletion. Together with the mineral crystalline condition of the magmatic hornblende, it is concluded that the hornblendite enclaves and their hosting diorites in the Jinling magmatic complex of intrusions may be produced by fractionation crystallization of cogenetic magmatic evolution, and the hornblendite enclaves crystalized from a lower magmatic chamber in the middle-crust level.

Key words: Jinling magmatic complex, hornblendite enclaves, the crystallization pressure of amphiboles, magmatic genesis, Western Shandong

摘要：

为了确定鲁西金岭岩浆侵入杂岩体中的角闪石岩包体成因, 对该类包体进行岩相学、矿物化学和地球化学分析。结果表明, 角闪石岩包体具有明显的堆晶结构, 主要由角闪石和少量斜长石组成。其中, 角闪石可以分为两类: 一类为韭闪石, 具有较低的SiO₂含量和较高的Al₂O₃含量, 是原生角闪石; 另一类为阳起石、镁角闪石和浅闪石, 相对富集SiO₂, 贫Al₂O₃, 可能为原生角闪石晚期被改造的产物。利用角闪石全铝地质压力计对原生角闪石进行压力计算, 获得其平均结晶压力为0.48 GPa。这些角闪石岩包体的微量元素特征与寄主岩石黑云母闪长岩相似, 均富集轻稀土元素, 亏损重稀土元素。结合原生角闪石的形成条件, 可以认为这些角闪石岩包体可能与寄主岩石同源, 是中地壳岩浆房闪长质岩浆分离结晶的产物。

关键词: 角闪石结晶压力, 岩浆成因, 鲁西地区, 金岭岩浆侵入杂岩体, 角闪石岩包体