天然气地球科学 ›› 2020, Vol. 31 ›› Issue (2): 268281.doi: 10.11764/j.issn.1672-1926.2019.10.016
杨晋东1(),赵峰华1(),秦胜飞2,邹雨1,宋昌贵1,孙宇翔1
Jin-dong YANG1(),Feng-hua ZHAO1(),Sheng-fei QIN2,Yu ZOU1,Chang-gui SONG1,Yu-xiang SUN1
摘要:
为探究燕山地区中元古界杨庄组碳酸盐岩物源及其构造沉积环境,采集研究区碳酸盐岩样品进行常微量元素(主要是稀土)地球化学测试,结合地质背景,通过地球化学分析得出如下
样品稀土含量(平均50.8×10-6)远高于纯白云岩(小于10×10-6),Al2O3与∑REE+Y呈显著正相关,且PAAS标准化稀土配分模式图呈平坦页岩型(除Eu的正异常),说明杨庄组碳酸盐岩受到显著陆源碎屑混染。杨庄组经历海侵海退旋回沉积,与Sr/Ba值和∑REE+Y值变化曲线相对应,暗示海平面升降控制陆源碎屑输入量;通过La/Sc—Th/Co、La/Yb—∑REE+Y和TiO2—Zr等关系图解和元素地球化学特征分析,结合华北克拉通北缘岩浆活动和构造演化,认为研究区的陆源碎屑最可能源于华北元古代大陆裂谷背景下形成的的酸性长英质火成岩类;杨庄组沉积相总体为潮上—潮间带,海水氧化性较强,不利于烃源岩的发育。
中图分类号:
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