首页> 外文期刊>Revue Roumaine de Geologie >PETROGENESIS OF THE SUSITA CALC-ALKALINE GRANITOIDS (SOUTH CARPATHIANS, ROMANIA)
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PETROGENESIS OF THE SUSITA CALC-ALKALINE GRANITOIDS (SOUTH CARPATHIANS, ROMANIA)

机译:SUSITA钙碱性颗粒(罗马尼亚喀尔巴阡山脉南部)的成岩作用

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摘要

The typical ratios of the major, minor and REE elements for the granitoid rocks, associated with the petro-mineralogical traits of the intrusions, within a tectonic setting, point out that the granodiorites (GRD), monzogranites (MZG) and syenogranites (SYG) are peraluminous, of S-type; the melanocrate diorites (Di) and the quartziferous diorites (QDi) are metaluminous, of Ⅰ-type. GRD, MZG and partially SYG are the result of the fusion of some mostly psammitic metasediments, coming from a continental crust. Di and QDi are the result of the mixing-mingling processes between the felsic crustal anatectic magmas and the basic magmas. The protolith of the basic magmas is represented by the subducted oceanic lithosphere or/and the upper mantle of the astenosphere.The main crystallisation phase and the intrusion of the Susita granitoids into the crystalline schists (Lainici-Paius Group) took place under collision-late collision tectonic conditions. In the final post-collision stage there followed a subsolidus, potassic hydrothermal episode, which led to the formation of SYG with shoshonitic trends, as well as of the migmatites of the Lainici-Paius Group. The source of this potassic pulsations is in the mafic component of the lower continental crust or, more likely, in the upper mantle.
机译:花岗岩的主要,次要和稀土元素的典型比例,与构造环境中侵入岩的岩石矿物学特征有关,指出了花岗闪长岩(GRD),单长花岗岩(MZG)和正长花岗岩(SYG)钙铝,S型;黑色素岩的闪长岩(Di)和石英质的闪长岩(QDi)是金属的,属于Ⅰ型。 GRD,MZG和部分SYG是来自大陆壳的一些主要是伪藻类沉积物融合的结果。 Di和QDi是长英质地壳食盐岩浆与基本岩浆之间混合混合过程的结果。基本岩浆的原石以俯冲的海洋岩石圈或/和涡流层的上地幔为代表。苏西塔花岗岩的主要结晶阶段和侵入进入晶体片岩(Lainici-Paius群)是在碰撞晚期发生的。碰撞构造条件。在最后的碰撞后阶段,发生了一个固相下的钾质热液事件,这导致了具有肖肖尼奇趋势的SYG以及Lainici-Paius群的辉贵岩的形成。钾离子脉动的来源是在下部大陆壳的铁镁质成分中,或更可能是在上地幔中。

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