首页> 外文期刊>Journal of the Geological Society of India >Heavy minerals and the characters of ilmenite in the beach placer sands of Chavakkad-Ponnani, Kerala Coast, India
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Heavy minerals and the characters of ilmenite in the beach placer sands of Chavakkad-Ponnani, Kerala Coast, India

机译:印度喀拉拉邦海岸查瓦卡德-波纳尼的沙滩砂中重矿物和钛铁矿的特征

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摘要

Indian beach placer sand deposits are, in general, ilmenite-rich. However, some concentrations are dominated by pyriboles. The Chavakkad-Ponnani (CP) area along the northern Kerala coast is one such deposit. This paper deals with the general character of the heavy minerals of CP with special emphasis on the characters of ilmenite. Most Indian beach sand ilmenites are of good quality. However, our observations on the ilmenites of CP using Optical Microscope, SEM and EPMA reveals that these are mineralogically very complex. The CP ilmenite varies from pure ilmenite to highly impure variety having intergrowths and inclusions of other oxide and silicate minerals. Ilmenite occurs as mixcrystals and forms intergrowth structure with hematite and Ti-hematite/ulv?spinel; contains inclusions of hematite, quartz, and monazite. On the other hand ilmenite also occurs as inclusions within hematite and garnet. The pyriboles are dominantly amphiboles with hornblende-composition. Interestingly an inclusion of gold has been recorded within amphibole of hornblende composition. Garnets are mostly of almandine and pyrope type. Subordinate heavy minerals are sillimanite, zircon and rutile. Characteristic morphology, mineralogy and chemistry of amphibole, garnet and ilmenite together indicate that the placer sands of CP area are derived from the amphibolites, granite gneisses and basic igneous rocks lying in the hinterland towards the eastern border of Kerala. Though the overall quality of ilmenite is poor, highgrade ilmenite concentrate can be generated (of course with lower yield), by adopting precise mineral processing techniques. The CP deposit can be considered as a second-grade deposit but it has potential for future exploitation.
机译:印度海滩砂砂沉积物通常富含钛铁矿。但是,某些浓度主要由吡唑决定。喀拉拉邦北部海岸的Chavakkad-Ponnani(CP)地区就是其中之一。本文探讨了CP重矿物的一般特征,特别是钛铁矿的特征。大多数印度沙滩钛铁矿的质量都很好。但是,我们使用光学显微镜,SEM和EPMA对CP钛铁矿的观察表明,它们在矿物学上非常复杂。 CP钛铁矿的种类从纯钛铁矿到高度不纯的品种,具有共生性和其他氧化物和硅酸盐矿物的夹杂物。钛铁矿以混合晶体的形式出现,并与赤铁矿和Ti-赤铁矿/ Ul?spinel形成共生结构。包含赤铁矿,石英和独居石的内含物。另一方面,钛铁矿也以赤铁矿和石榴石的夹杂物形式存在。吡咯主要是角闪石组成的闪石。有趣的是,在角闪石成分的闪石中已记录了金的含量。石榴石主要是金刚烷和吡啶型的。次要重矿物为硅线石,锆石和金红石。闪石,石榴石和钛铁矿的特征形态,矿物学和化学性质共同表明,CP地区的砂矿砂来自内陆腹地的喀拉拉邦东部边界的角闪石,花岗岩片麻岩和基本火成岩。尽管钛铁矿的整体质量很差,但通过采用精确的选矿技术,可以生成高品位的钛铁矿精矿(当然产率较低)。 CP矿床可以被认为是二级矿床,但它有可能被将来开采。

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