藏东贡觉盆地白垩纪末期风成沉积组合及其古气候和古地理意义*
杜研1,2, 许欢1,2, 丁家翔1,2, 何柯衡1,2, 赵潇然1,2, 夏磊3, 苑婷媛2,4, 张毕辉1,2, 刘高政1,2

Late Cretaceous aeolian sedimentary association in Gonjo Basin, eastern Tibet: implications for palaeoclimate and palaeogeography
DU Yan1,2, XU Huan1,2, DING Jiaxiang1,2, HE Keheng1,2, ZHAO Xiaoran1,2, XIA Lei3, YUAN Tingyuan2,4, ZHANG Bihui1,2, LIU Gaozheng1,2
藏东贡觉盆地贡觉组底部水成沉积特征宏观露头特征 a—沃木杂村风成沉积剖面; b—与泥石流沉积层接触的颗粒流层; c—风成沉积与水成沉积接触区; d—混杂堆积的泥石流沉积;e—风成沉积与水成沉积交互类型一; f—风成沉积与水成沉积交互类型二; g—f中黄色阴影块的放大图; h—微弱的软沉积变形构造