论文部分内容阅读
马来西其西部锡矿床存空间分布上与出露的花岗岩密切相关,并显然分成两个主要矿带,其一与曼因山脉伴生,其二与东海岸的花岗岩伴生。矿床多半位于主要酸性侵入体两侧,完全在花岗岩接触带内侧的矿体少而小;沿花岗岩侵入体接触带,矿床分布不稳定,就曼因山脉区而言,其西侧的锡矿化发育程度比东侧强得多。在东带,从经济价值的观点来说,彭亨联合矿山的原生矿床大大超过这里已知的任何其他矿床。
The distribution of the tin deposits in western Malaysia is closely related to the exposed granite. It is apparently divided into two main ore zones, one of which is associated with the Man-En-sierra and the other with the granites on the east coast. The deposits are mostly located on both sides of the main acid intrusion, and the ore bodies completely inside the granite contact zone are small and small. Along the granite intrusive contact zone, the deposits are not stable. For the Man Mountain range, the tin mineralization on the west side The development is much stronger than the east. From the point of view of economic value, in the east belt, the primary deposits of the Pahang coal mine vastly outperform any other deposits known here.