[1] .Nemec W, Steel R J. Alluvial and coastal conglomerates: their significant features and some comments on gravelly mass-flow deposits. In: Koster E H, Steel R J, eds. Sedimentology of Gravels and Conglomerates. Canadian Society of Petroleum Geologists Memoir, 1984, 10: 1～31
[2] .Visher G S. Grain size distribution and depositional processes. J. Sed. Petrology, 1969, 39: 1074～1106
[3] .Glaister R P, Nelson HW. Grain-size distribution, an aid in facies identification. Bulletin of Canadian Petroleum Geology, 1974, 22(3): 203～240
[4] .Kochel R C, Johnson R A. Geomorphology and sedimentology of humid-temperate alluvial fans, central Virginia. In: Koster E H, Steel R J, eds. Sedimentology of Gravels and Conglomerates. Canadian Society of Petroleum Geologists Memoir, 1991, 10: 109～122
[5] .柯宝嘉, 陈昌明, 陈志明等. 鄂尔多斯盆地西缘砾质冲积扇沉积学特征. 沉积学报, 1991, 9(3): 11～21
[6] .Middleton G V. Experimental studies related to flysh sedimentation. In: Lajoie, eds. Flysh Sedimentology in North America, 1970, 253～272
[7] .Bhattacharjee C C. The ophiolites of northeast India-a subduction zone ophiolite complex of the India- Burman orogenic belt. Tectonophgysics, 1991, 191: 213～222
[8] .吴根耀. 中国滇西—泰国地区侏罗纪—第四纪盆地发育对比研究. 地质科学, 1991, (4): 359～368
[9] .吴根耀. 滇西北地区第三纪的逆冲—推覆构造. 大地构造与成矿学, 1994, 18(4): 331～338
[10] .钟大赉, 丁林. 青藏高原的隆起过程及其机制的探讨. 中国科学(D辑), 1996, 26(4): 289～295
[11] .刘善印, 钟大赉, 吴根耀. 滇西南晚第三纪含煤盆地的形成与演化. 煤炭学报, 1995, 20(4): 351～355