2011•Geology of AnhuiRequires access

METALLOGENY OF TERRESTRIAL VOLCANIC ORE DEPOSITS IN ORE BELT ALONG THE MID-LOWER YANGTZE RIVER REACH

MA Xiao-hong

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Abstract

Based on study of geological setting of metallogenic belt along the mid-lower Yangtze River reach,metallogenic comparison between the Ning-Wu and Lu-Zong basins,it is argued that the iron ore deposit in the Mesozoic terrestrial volcanic basin and its periphery in the area has a double-layer ore-control structurethat consists of the upper part of porphyry iorn ore and the lower part similar to Dayeiron ore.Regional iron ore-forming law was summarized and major direction shown for further iron ore exploration in the area.

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Based on study of geological setting of metallogenic belt along the mid-lower Yangtze River reach,metallogenic comparison between the Ning-Wu and Lu-Zong basins,it is argued that the iron ore deposit in the Mesozoic terrestrial volcanic basin and its periphery in the area has a double-layer ore-control structurethat consists of the upper part of porphyry iorn ore and the lower part similar to Dayeiron ore.Regional iron ore-forming law was summarized and major direction shown for further iron ore exploration in the area.

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Available abstract

Based on study of geological setting of metallogenic belt along the mid-lower Yangtze River reach,metallogenic comparison between the Ning-Wu and Lu-Zong basins,it is argued that the iron ore deposit in the Mesozoic terrestrial volcanic basin and its periphery in the area has a double-layer ore-control structurethat consists of the upper part of porphyry iorn ore and the lower part similar to Dayeiron ore.Regional iron ore-forming law was summarized and major direction shown for further iron ore exploration in the area.

Key concepts: Metallogeny, Geology, Iron ore, Geochemistry, Volcano, Structural basin, Yangtze river, Ore genesis

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