斯里兰卡西南部近海矿产的近岸地球物理调查

G. Sonnichsen, J. Lewis, N. P. Wijayananda, G. A. Nooten
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引用次数: 0

摘要

1997年,加拿大地质调查局(大西洋)在斯里兰卡西南部近岸进行了高分辨率海洋地球物理调查,以确定颗粒沉积物的分布、沉积环境和估计体积。这项调查是确定重矿物经济集中度的第一步。地球物理设备包括Simrad侧扫声纳系统、IKB seisstec海底剖面仪和Knudsen工程公司的320M回声测深仪。68个抓取样本提供了解释的海底单元的选择性地面真值。地球物理资料分析量化了可采颗粒沉积物的厚度和体积。确定了11个潜在的颗粒资源点。估计的泥沙体积范围从2/spl倍/10/sup 6/ m/sup 3/到120/spl倍/10/sup 6/ m/sup 3/以上。根据伽马射线能谱分析,估计独居石浓度高达1.1%。没有关于重矿物地下浓度的资料。1997年的海洋地球物理结果使地貌和沉积物分布的广义模型得以发展。通过对现代重矿砂富集机制的了解,提出了内陆架地质演化过程中的侵位假说。该模式有助于查明经济重矿物储量前景最高的资源地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A nearshore geophysical survey for offshore minerals, southwestern Sri Lanka
In 1997, the Geological Survey of Canada (Atlantic) conducted a high-resolution marine geophysical survey in the nearshore off southwestern Sri Lanka to determine the distribution, depositional environment and estimated volumes of granular sediment. The survey was the first step to identifying economic concentrations of heavy minerals. Geophysical equipment included a Simrad sidescan sonar system, an IKB Seistec subbottom profiler, and a Knudsen Engineering Ltd., 320M echo sounder. Sixty-eight grab samples provided selective ground truth of the interpreted seabed units. Analysis of the geophysical data quantified the thickness and volume of recoverable granular sediments. Eleven potential granular resource sites were identified. Estimated sediment volumes ranged from 2/spl times/10/sup 6/ m/sup 3/ to more than 120/spl times/10/sup 6/ m/sup 3/. Monazite concentrations as high as 1.1% were estimated based on gamma ray spectrometry analysis. No information exists on the subsurface concentration of heavy minerals. The 1997 marine geophysical results enabled development of a generalized model of the geomorphology and sediment distribution. Understanding the mechanisms of modern concentration of heavy mineral sands were used to develop hypotheses of emplacement during the geological evolution of the inner shelf. The model assists in identifying resource areas with the highest prospects for economic heavy mineral reserves.
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