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淮北煤矿塌陷区湿地生态环境营建及旅游产品开发 总被引：2，自引：0，他引：2
煤矿塌陷区生态环境治理一直是一个关系国计民生的难题。近年来,淮北市对煤矿塌陷区形成的大面积湿地进行大力整治,经过近20年努力,建成我国第一个煤矿塌陷区国家级城市湿地公园,将昔日荒凉的废弃地变成了生态旅游天堂。对淮北煤矿塌陷区生态环境营建进行分析总结,对其生态旅游产品开发提出了建议。 相似文献
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现有湿地公园仅对湿地公园个案进行研究,研究结果难以上升到理论高度,探索了利用比较研究的方法研究湿地公园。通过对杭州西溪、黄山太平湖和淮北南湖3个国家级湿地公园建设情况和生态旅游发展的SWOT分析与比较研究,指出了湿地公园建设中存在的问题及其生态旅游发展的优势和劣势、面临的机遇和挑战,对湿地公园的建设和生态旅游发展提出了对策和建议。 相似文献
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Contributions to Mineralogy and Petrology - New geochemical data demonstrate the similarity between Neoarchaean TTGs found in the middle crust of the Zimbabwe Craton and the lower crust of the... 相似文献
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Qiu-Huan Li Yu-Xiu Zhang Li-Long Yan Lu Zeng Xin Jin 《International Geology Review》2018,60(16):1954-1967
The Ganzi–Litang fault zone, an outstanding tectonic element in the eastern Tibetan Plateau has been intensively debated as an in-situ suture zone marking relict of a subducted Palaeo-Tethyan oceanic crust or a failed intracontinental rift. This paper reports the garnet amphibolites discovered along the Ganzi–Litang fault zone, eastern Tibetan Plateau. These garnet amphibolites are characterized by the garnet–hornblende–rutile–sphene–plagioclase–quartz assemblage. Conventional geothermobarometry figures out the metamorphic temperature and pressure conditions at 582–626°C and 1.61–1.82 GPa, respectively. Geochemical analysis (no Nb–Ta deletions and left-inclined to flat patterns of rare-earth elements) indicates that the garnet amphibolites could represent metamorphic product of the mid-ocean-ridge (MORB)-type mafic rocks that were contaminated by a mantle plume. The protolith of the garnet amphibolites was dated at 236 Ma using in-situ U–Pb zircon method, and the retrograde metamorphism was dated at 218 Ma using in-situ U–Pb sphene method. A comprehensive analysis combined with the development of the Palaeo-Tethys Ocean and the Yidun arc through geologic time indicates a Triassic to Early Jurassic age (236–195 Ma) for the metamorphism of the garnet amphibolites. The low geothermal gradient of 9.8ºC/km and the N-MORB nature of the garnet amphibolites suggest a subduction-zone environment for the high-pressure metamorphism. Therefore, the Ganzi–Litang fault zone is a Palaeo-Tethyan suture separating the Yidun arc and the Songpan–Ganzi terrane, representing the relics of a branch of the Palaeo-Tethys Ocean that was contaminated by a mantle plume. 相似文献
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