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陈森强 《资源导刊(河南)》2024,(4):29-32+37
卫星遥感作为一种直观、可量化的监测手段,在矿山修复和生态文明建设中产生了广泛应用。基于Google Earth Engine(GEE)平台,利用遥感生态指数来时序量化评价西江锰矿修复区内生态环境质量。从2015年至2021年期间监测区的RSEI空间分布来看,由于西江锰矿区内生产作业强度不断加大,矿坑裸露范围持续扩大,导致矿区内生态质量趋坏;而2021年的RSEI分布显示,监测区内的生态环境逐渐改善,尤其是已经进行系统恢复的区域,生态环境状况已经达到未开采前的水平,生态修复效果良好。研究成果可为西江锰矿区生态环境工程建设实施和评价提供科学依据。 相似文献
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GEOTECTONICS CHARACTERISTICS AND THEIR RELATION WITH GAS-OIL POOL FORMATION OF THE DONGSHA FAULT-UP LIFTED MASSIF 总被引:1,自引:0,他引:1
The Dongsha fault- uplifted massif (for convenience . Dongsha massif from here on) is located in the northern continental shelf-slope of the South China Sea, where the water depth is 100-400m. The massif is considered to be a part of the large-scale fault-uplifted zone directed NE and separating the Pearl River Mouth Basin into northern and southern graben areas. The sedimentary cover of the Pearl River Mouth Graben consists mainly of a 7000-10000m thick Tertiary system. A large-scale uplift occurred in the Dongsha fault-uplifted zone during Paleocene-Eocene when the lower structural layer (lower Tertiary) existed only in the small depressions of the fault-uplifted zone. The formation and evolution of the Dongsha fault-uplifted zone could be divided into: 1) the basement formation stage (J2-K1); 2) the slowly uplifted stage (K2-E22); 3) the weathering and erosion stage (E23-E31); 4) the integrated subsidence stage (E32-N12) and 5) the last uplifted stage (N13-Q). The formation of the oil and gas pools o 相似文献
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