1.闫小兵,周永胜,杨晓松,2007,人工地震反射法在超前地质预报中的应用,地震地质,29(4):894-904
2.王多君,马瑾,杨晓松,周平,2007,地幔矿物电导率研究进展,地震地质,29(1):152-160
3.Yang Xiaosong,Zhou Ping,Ming Yuehong,2007,Vp of muscovite-biotite gneiss up to 950°C at 400 Mpa:Constraints on the origin of abnormal seismic layers in continental crust, Chinese Science Bulletin,52(24):3397-3402
周平,杨晓松,王多君,2006,熔体形态学及其对岩石物理和力学性质的影响,地球物理学进展,21 (3):790-797
4.YANG Xiaosong,JIN Zhenmin,MA Jin. 2005. Anatexis in Himalayan crust:Evidence from geochemical and chronological investigations of Higher Himalayan Crystallines. Science in China(Series D), 48(9):1347-1356.
5.Yang, X. S., Du, S, Ma, J. 2004. Do Earthquakes Exhibit Self-Organized Criticality. Physics Review Letters, 92: 228501 -228504.
6.杨晓松, 金振民, 马瑾. 2004. 喜马拉雅造山带地壳深熔作用: 来自聂拉木群混合岩的地球化学和年代 学证据. 中国科学D 34: 926-934.
7.杨晓松, 马瑾, 刘力强. 2004. 周期性层状介质中超声波传播的实验研究. 地震地质, 26(3): 484-491.
8.Yang Xiaosong, Ma Jin, Jin Zhenmin, Gao Shan and Ma Shengli. 2003. Partial melting and its implications for understanding the seismic velocity structure with the southern Tibetan Crust. Acta Geologica Sinica, 77(1): 64-71.
9.杨晓松, 马瑾. 2003. 大陆岩石圈解耦及块体运动讨论—以青藏高原—川滇地区为例.地学前缘, 10(特刊): 240-247.
10.杨晓松,马瑾,张先进. 2003. 大陆壳内低速层成因. 地质科技情报, 22(2):35-41.
11.yang Xiaosong, Jin Zhenmin, Gao Shan, Huenges E. 2002. Genesis of Granulite in Himalayan Lower Crust: Evidences from Experimental Study at High Temperature and High Pressure. Chinese Science Bulletin, 47(6): 448-453.
12.杨晓松,金振民,马瑾, Huenges E., Schilling F. 2002. 青藏高原北部异常SKS分裂成因的初步探讨―被熔体强化的岩石圈各向异性. 地球物理学报, 45(6): 821-831.
13.Yang X S, Jin Z. M., et al., Experimental study on dehydration melting of natural biotite-plagioclase gneiss from high Himalayas and implications forHimalayancrust anatexis, Chinese Science Bulletin, 2001, 46(10):867-871.
14.杨晓松, 金振民, 高山, E. Huenges等. 2001. 喜马拉雅造山带下地壳麻粒岩成因: 来自高温高压实验的证据. 科学通报, 46(24): 2025-2030.