新疆博格达地区中二叠世—早三叠世构造-气候-沉积演化及耦合机制*
史燕青1,2, 王剑3, 张国一4, 刘明3, 向鹏飞1,2, 杨志波1,2, 季汉成1,2

Tectono-climatic-sedimentary evolution and coupling mechanism during the middle Permian-early Triassic in Bogda area,Xinjiang
Shi Yan-Qing1,2, Wang Jian3, Zhang Guo-Yi4, Liu Ming3, Xiang Peng-Fei1,2, Yang Zhi-Bo1,2, Ji Han-Cheng1,2
新疆博格达地区中二叠统平地泉组(红雁池组)—下三叠统韭菜园子组岩石类型及沉积构造 a—波痕,红雁池剖面中二叠统红雁池组;b—厚层碳质泥岩,柴窝堡剖面中二叠统红雁池组;c—含黄铁矿砂岩,乌鲁木齐剖面中二叠统红雁池组;d—冲刷面,中二叠统平地泉组;e—软沉积物变形,中二叠统平地泉组;f—砾岩,博格达山北缘上二叠统梧桐沟组;g—B19井,2058.32 m,砾岩,上二叠统梧桐沟组;h—B84井,2694.13 m,凝灰质角砾岩,上二叠统梧桐沟组;i—定向排列砾石,吉木萨尔西大龙口剖面下三叠统韭菜园子组;j—砾岩,F19井,2675.25 m,下三叠统韭菜园子组;k—冲刷构造,B53井,2345.07 m,下三叠统韭菜园子组;l—平行层理,XQ9井,2599.54 m,下三叠统韭菜园子组;m—泥裂冲刷,XQ11井,3137.89 m