碎屑岩脉

碎屑岩脉（英语：clastic dike）是沉积物充填到岩石裂缝中的岩脉。碎屑岩脉通过液化注入（加压孔隙流体的流动）或通过水、风和重力的沉积形成^[1]。碎屑岩脉通常是垂直的或接近垂直的。厘米级宽度很常见，但厚度范围从毫米到米。长度通常是宽度的许多倍。在全世界的沉积盆地沉积物中都发现了碎屑岩脉^[2]^[3] ^[4]。

参考文献

^ Davies, Richard J.; Huuse, Mads; Hirst, Philip; Cartwright, Joe; Yang, Yuesuo (2006). "Giant clastic intrusions primed by silica diagenesis". Geology. 34 (11): 917. Bibcode:2006Geo....34..917D. doi:10.1130/G22937A.1.
^ Diller, J.S., 1890, Sandstone dikes, GSA Bulletin, 1, p. 411-442
^ Cross, W., 1894, Intrusive sandstone dikes in granite, GSA Bulletin, 5, p. 225-230
^ Crosby, W.O., 1897, Sandstone dikes accompanying the great fault of Ute Pass, Colorado, Essex Institute Bulletin, 27, p. 113-147

[”Davies”-1] Davies, Richard J.; Huuse, Mads; Hirst, Philip; Cartwright, Joe; Yang, Yuesuo (2006). "Giant clastic intrusions primed by silica diagenesis". Geology. 34 (11): 917. Bibcode:2006Geo....34..917D. doi:10.1130/G22937A.1.

[”Diller”-2] Diller, J.S., 1890, Sandstone dikes, GSA Bulletin, 1, p. 411-442

[”Cross”-3] Cross, W., 1894, Intrusive sandstone dikes in granite, GSA Bulletin, 5, p. 225-230

[”Crosby”-4] Crosby, W.O., 1897, Sandstone dikes accompanying the great fault of Ute Pass, Colorado, Essex Institute Bulletin, 27, p. 113-147

[1]

[2]

[3]

[4]