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摘 要:阐述了砂质碎屑流沉积特征、研究现状及其与其他深海碎屑沉积的区别,认为西藏特提斯喜马拉雅上休罗统-下白垩统深海沉积背景下的块状砂岩具有砂质碎屑流沉积性质,指出深海相中的块状砂岩可以预测。
关键词:砂质碎屑流;块状砂岩;深海相;上休罗统-下白垩统;西藏特提斯喜马拉雅
基金项目:国家杰出青年科学基金(49625203)项目
作者简介:李祥辉 男 35岁 副教授 沉积学专业 研究方向:层序地层学和喜马拉雅地质
作者单位:李祥辉(成都理工学院沉积地质研究所,成都 610059)
王成善(成都理工学院沉积地质研究所,成都 610059)
胡修棉(成都理工学院沉积地质研究所,成都 610059)
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