关于赣中相山矿田相山“碎斑熔岩”
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本文受核工业北京地质研究院“相山矿田西北部不同成矿类型比较研究和远景评价”项目资助。


On the Xiangshan “Porphyroclastic Lava” in Xiangshan Orefield, Central Jiangxi
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    摘要:

    赣中相山矿田相山杂岩体的主体岩石——“碎斑熔岩”的成因和命名,长期看法不一,主要观点有火山喷发成因、火山溢流成因、火山侵出成因、潜火山侵入成因等,本文通过综述“碎斑熔岩”的岩石学和相带特征,结合剥蚀程度、密度垂向变化研究成果,论述了“碎斑熔岩”不是火山岩而是侵入岩的成因观点。同时,对相山是否存在潜火山岩提出了质疑,探讨了相山“碎斑熔岩”的形成深度问题。认为“碎斑熔岩”命名为碎斑花岗斑岩更符合其侵入成因特点。

    Abstract:

    The genesis of the “porphyroclastic lava”, principal rock of the Xiangshan complex in the central Jiangxi Province, has been debated for a long time. Main considerations are volcanic eruption, volcanic overflow, volcano extrusion or subvolcanic intrusion, etc. Based on an integrated analysis of petrology and the characteristics of facies, in combination with existed studies about erosion degree and the vertical change of density of the “porphyroclastic lava”, writers propose an intrusion genesis viewpoint, i. e. the “porphyroclastic lava” is not the production of volcanic rock, but the intrusive rock. Meanwhile, writers put out a question that whether has subvolcanic rocks in the Xiangshan area, and discuss the formation depth of the “porphyroclastic lava”. In conclusion, writers consider that the “porphyroclastic lava” should be named as porphyroclastic porphyry, which accords better with its intrusive genesis characteristics.

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张万良,李子颖.2015.关于赣中相山矿田相山“碎斑熔岩”[J].地质论评,61(2):367-375,[DOI].
ZHANG Wanliang, LI Ziying.2015. On the Xiangshan “Porphyroclastic Lava” in Xiangshan Orefield, Central Jiangxi[J]. Geological Review,61(2):367-375.

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  • 收稿日期:2013-12-01
  • 最后修改日期:2015-01-05
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  • 在线发布日期: 2015-03-22
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