[17]中国地质大学学报(自然科学版),2016,第2期,第1 -第2期

A. T. Joseph, A. Vatuva, J. Indongo
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引用次数: 0

摘要

位于纳马夸-纳塔尔变质省(NNMP)的纳马夸板块正在进行的研究对于了解罗迪尼亚超大陆组合期间发生的地质活动至关重要。这些地质活动通常是发现新矿物原料的关键。Tschaukaib花岗岩套产于Tschaukaib山脉内部,被认为是Kakamas域Gordonia逆冲叠层(GTS)的一部分,通过地表填图、岩石学和主要元素地球化学研究对其进行了表征。鉴定出3种花岗岩类型:花岗闪长岩、石英二长岩和花岗岩,SiO2含量为64.9 ~ 69.8%。全岩地球化学进一步表明,它们是钙碱性、碱钙性、铁质、过铝(Al2O3 > K2O + Na2O + CaO),具有> %的Cross、Iddings、Pirsson和Washington (CIPW)刚玉。地球化学特征表明,花岗岩类岩体形成于大陆碰撞时期,由罗迪尼亚超大陆时期的地壳物质部分熔融而成。地球化学特征显示出明显的分馏结晶特征。Tschaukaib花岗岩套区地质填图和构造分析显示,Tschaukaib奥根片麻岩(石英二长岩)呈NW-SE和E-W走向的区域片理构造,对应于D2次主纳马夸变质事件。绘制了几个剪切带,与研究区平行的北西—东南、东西—西走向的Pofadder剪切带一致。岩石学分析发现花岗岩类的矿物组合表明花岗岩类经历了高应变和高蚀变,但尚不清楚是哪一次纳马夸变形事件造成了这些特征。
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77Namibian Journal forResearch, Science andTechnologyVol 2, December2020NJRST 2 (2020): 77-89 Geological Mapping and Major Elements Characterization of the Tschaukaib Granitic Suite, South West Namibia
ABSTRACTOngoing studies in the Namaqua Sector, situated in the Namaqua-Natal Metamorphic Province (NNMP), have been vital in understanding the geological activities that occurred during the Rodinia supercontinent assembly. These geological activities are usually key to discovering new mineral raw materials. The Tschaukaib Granitic Suite, which is believed to be part of the Gordonia Thrust Stack (GTS) of the Kakamas Domain, crops out within Tschaukaib Mountains and was characterized in this study on the basis of surface mapping, petrographic and major element geochemistry. Three types of granites were identified, namely: granodiorite, quartz monzonite and granite with SiO2 content ranging from 64.9 wt % to 69.8 wt %. Whole rock geochemistry further shows that they are calc-alkaline, alkali-calcic, ferroan, peraluminous (Al2O3 > K2O + Na2O + CaO) and have >1 % Cross, Iddings, Pirsson and Washington (CIPW) corundum. The geochemical characteristics indicates that the granitoids were emplaced during the continental collision and are formed from partial melting of recycled crustal material which took place during the Rodinia supercontinent. The geochemistry shows a conspicuous fractional crystallization signature. Geological mapping and structural analysis of the Tschaukaib Granitic Suite area shows a NW-SE and E-W trending regional foliation in the Tschaukaib Augen Gneiss (quartz monzonite) which corresponds to the main D2 Namaqua metamorphic event. Several shear zones were mapped and are consistent to the Pofadder Shear Zone which runs in the NW-SE and E-W directions, parallel to the study area. Petrographic analysis of the granitoids has identified mineral assemblages which shows that the granitoids have undergone high strain and alterations, however, it is not clear which Namaqua deformation episode brought about these features.
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