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甘肃北山三个井组碎屑岩地质、地球化学特征及其沉积构造背景
引用本文:翁凯,张雪,梁积伟.甘肃北山三个井组碎屑岩地质、地球化学特征及其沉积构造背景[J].地质找矿论丛,2013,28(3):434-440.
作者姓名:翁凯  张雪  梁积伟
作者单位:1. 长安大学地球科学与资源学院,西安710054;西安地质矿产研究所,西安710054
2. 长安大学地球科学与资源学院,西安,710054
基金项目:由项目"西北基础地质调查成果集成与综合研究","北山—祁连成矿带地质矿产综合研究"
摘    要:为查明甘肃北山地区三个井组沉积岩的物质来源和形成背景,通过对该地层砾岩和粗砂岩进行野外观察和镜下鉴定,分析细砂岩和泥岩的地球化学特征,认为三个井组沉积岩物质成分复杂,分选磨圆中等,具有快速堆积的特征;沉积物质主要来源于火山岛弧和活动大陆边缘遭受剥蚀的造山带,沉积区具有周缘前陆盆地的特征。

关 键 词:三个井组  沉积岩  地球化学特征  构造背景  北山地区  甘肃省
收稿时间:2012/12/24 0:00:00

Geological and geochemical characteristics of clastic rock in the Three Wells Formatrion in Beishan area, Gansu
WENG Kai,ZHANG Xue and LIANG Jiwei.Geological and geochemical characteristics of clastic rock in the Three Wells Formatrion in Beishan area, Gansu[J].Contributions to Geology and Mineral Resources Research,2013,28(3):434-440.
Authors:WENG Kai  ZHANG Xue and LIANG Jiwei
Institution:WENG Kai;ZHANG Xue;LIANG Jiwei;School of Earthscience & Resources,Chang’an University;Xi’an Institute of Geology and Mineral Resources;
Abstract:In order to find out material sources and rock-forming background of sedimentary rock in the three wells formation in Gansu Beishan area, the detailed field observation and microscopic identification were made on the conglomerate and grit in the formation and and geochemical characteristics of the fine sandstone and mudstone are analysed. It is considered that the Three Wells Formation is complicated in source materials with medium sorting grinding and quick accumulation. The swedimentary materials mainly come from volcanic island arc and active continental marginal orogenic belts and the sedimentation area is characterized by the marginal foreland basin.
Keywords:the Three wells Formation  sedimentary rock  geochemical characteristics  tectonic background  Gansu province
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