[1] 肖思云,张维吉,宋子季,1988,北秦岭变质地层,西安:西安交通大学出版社。
[2] 于在平,孙勇,张成立,Altenberger, U.,1981,秦岭商丹缝合带变质砂岩地球化学特及构造环境探讨,地质论评,37(6) ; 492~507.
[3] 张国伟,1991,试论秦岭造山带岩石圈构造演化基本特征,西北大学学报,21(2) : 77-87.
[4] Dickinson,W. R. and Seely/y,D. R.,1979, Structure and stratigraphy of fore一arc regions, Bull,Am.Assoc. Pet. Geol.,V.63,p.2~31.
[5] Fisher, R. V.,1971, Features of coarse一grained, high一concentration fluids and their deposits. J. Sediment.Petrol., V. 91, p. 916一927.
[6] Fisher, R. V.,1983,F1ow transformations in sediment gravity flow. Geology,V. 11,p. 273~274.
[7] Hampton, M. A.,1972,The role of subaqueous debris flow in generating turbidity currents. J. Sediment.Petrol. V. 92, p. 775一739.
[8] Hampton, M. A.,1975,Competence of fine一grained debris flows. J. Sediment. Petrol., V. 45, p. 834一899.
[9] Johnson, A. M.,1970.Physical processes in geology. Freeman,Cooper and Co.,San Francisco.
[10] Karig, D. E. and Sharman, G. F.,1975, Subduction and accretion in trenches, Geol. Soc. Am. Bull., V. 86, p.377-389.
[11] Lowe,D.R.,1976,Grain flow and grain flow deposits,J. Sediment. Petrol. V. 46,P. 188~199.
[12] Lowe,D. R.,1982,Sediment gravity flow:1 .Depositional models with special references to the deposit of high一density tubidity currents. J. Sediment. Petrol., V. 52,p. 279一297.
[13] Naylor, M. A.,1980,The,on琪n of inverse grading in muddy debris flow deposits一a review. J. Sediment.Petrol.,V.50,p. 1111~1116.
[14] Nemec, W. and Stee1,R. J.,1989,Alluvial and coastal conglomenrates;their significancant features and some comments on gravelly mass一flow deposits, Can. Soc. Petrol. Geol.,Mem. 10,p. 1~31.