夾石 (地質學)
夾石（英語：）在地質科學是指一塊岩體，被礦脈或斷層面與周圍岩石完全隔離的任何岩石塊。 在採礦業中，該詞是指一塊完全包裹在礦脈中的圍岩[1]。在構造地質學中，該詞首先用於描述一塊疊瓦狀岩體被逆衝斷層包圍的岩石[2]。 後來，它已成為任何完全由斷層包圍的岩體的總稱，不論它的變形是在擠壓、伸展或是走滑性構造環境造成的[3][4]。
參考文獻
- Butler, F.H. 1911. The brecciation of mineral veins
- Dennis, J.G. 1967. International tectonic dictionary. AAPG Memoir 7, 196pp.
- Root, K.G. 1990. Extensional duplex in the Purcell Mountains of southeastern British Columbia. Geology, 18, 419-421
- Laney, Stephen E; Gates, Alexander E (1996), "Three-dimensional shuffling of horses in a strike-slip duplex: an example from the Lambertville sill, New Jersey", Tectonophysics, 258 (1–4): 53–70, doi:10.1016/0040-1951(95)00173-5
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