吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 650-661.doi: 10.13278/j.cnki.jjuese.20180071
赵佳琦1, 高有峰2,3, 刘海波1, 王清斌4, 张艳1, 王璞珺1,2
Zhao Jiaqi1, Gao Youfeng2,3, Liu Haibo1, Wang Qingbin4, Zhang Yan1, Wang Pujun1,2
摘要: 通过对总长2 705 m两条剖面的实测、40块薄片鉴定、419个砾石统计及其粒度分析,确定了辽西地区北票盆地中侏罗统海房沟组砾岩的沉积特征及成因。研究表明:辽西北票盆地海房沟组主要岩性为一套冲积扇相的复成分砾岩,并夹一套喷溢相下部亚相安山质角砾熔岩和另一套爆发相空落亚相安山质角砾凝灰岩、热碎屑流亚相安山质角砾凝灰熔岩;海房沟组沉积物源来自研究区SSW向的太古宇变质岩及结晶基底和下侏罗统兴隆沟组火山岩的全面快速隆升剥蚀。结合构造背景,通过对北票组与海房沟组界线的研究和岩性岩相的鉴定,确定海房沟组冲积扇相的复成分砾岩是燕山运动二期挤压伸展构造运动的重要产物,两套中酸性火山岩的出现是两次火山喷发的重要标识。
中图分类号:
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