碎屑岩脈

碎屑岩脈（英語：clastic dike）是沉積物充填到岩石裂縫中的岩脈。碎屑岩脈通過液化注入（加壓孔隙流體的流動）或通過水、風和重力的沉積形成^[1]。碎屑岩脈通常是垂直的或接近垂直的。厘米級寬度很常見，但厚度範圍從毫米到米。長度通常是寬度的許多倍。在全世界的沉積盆地沉積物中都發現了碎屑岩脈^[2]^[3] ^[4]。

參考文獻

^ 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

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