关于赣东北上墅组火山岩的再认识及其地质意义
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New Knowledge about The Volcanic Rocks of Shangshu Formation from Northeastern Jiangxi Province and Their Geological Significance
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    摘要:

    本论文对与我国南方板溪群相当的赣东北上墅组火 山岩进行了地 质学、岩石学、地球化学和定年研究。提出该火山岩应划分为形成时代不同、岩石特征各异 的两大类型:其一为红色陆相中、新元古代钙碱性中—高钾火山岩和碱性钾玄岩;其二为绿 色海相早、中古生代拉斑玄武质低—中钾火山岩。笔者认为,赣东北地区原定的板溪群(古 陆)应当解体,其中的红色陆相火山岩系为所谓的江南古陆的一部分,可与我国东南的板溪 群相当;绿色的海相火山岩系则不属于板溪群,应从江南古陆中分解出来。

    Abstract:

    The thesis has reseached on geology. petrology, geochemistry a nd chronology for Shangshu volcanic rocks that corespond to the Banxi formation in the upper proterozoic subera. It is proposed that this volcanic rocks were di vided into two group: first one is the red subaerial cakealkalic mediumhigh potossium volcanic rocks and alkaline shoshonite that were formed in middleupp er proterozoic era; second one is the green submarine lowmedium potossium thol eiitic volcanic rocks that were formed in the middlelower palaeozoic era. It is recognize that the Banxi formation represented the ancient continent from northeastern Jiangxi province must be resolved: the red subaerial volcanic rocks is a part of Jiangnan ancient continent, it corespond to Banxi formation; but th e green submarine volcanic rocks not belong to the Banxi formation and must sep arate from Jiangnan ancient continent.

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李昌年,廖群安.1999.关于赣东北上墅组火山岩的再认识及其地质意义[J].地质论评,45(7):717-723,[DOI].
Li Changnian, Liao Qun′an.1999. New Knowledge about The Volcanic Rocks of Shangshu Formation from Northeastern Jiangxi Province and Their Geological Significance[J]. Geological Review,45(7):717-723.

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