Static versus dynamic fracturing in shallow carbonate fault zones

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• 作者：Michele Fondriest^a ; ^{michele.fondriest@manchester.ac.uk} ; Mai-Linh Doan^b ; Frans Aben^b ; Florian Fusseis^c ; Tomas M. Mitchell^d ; Maarten Voorn^e ; ¹ ; Michele Secco^f ; ^g ; Giulio Di Toro^a ; ^h ; ⁱ
• 关键词：in-situ shattering ; dynamic loading ; earthquakes ; quasi-static loading ; carbonates ; fractures
• 刊名：Earth and Planetary Science Letters
• 出版年：2017
• 出版时间：1 March 2017
• 年：2017
• 卷：461
• 期：Complete
• 页码：8-19
• 全文大小：4194 K
• 卷排序：461

文摘

In-situ shattering is the result of high-energy dynamic rock fragmentation. Quasi-static and dynamic fracture patterns are significantly different. Experimental in-situ shattered dolostones resemble the natural ones. In-situ shattered dolostones are geological markers of earthquake ruptures.