深成岩
深成岩,是侵入火成岩,位于地壳的较大深度(>2 km),在地下缓慢冷却使得矿物具有大的结晶粒度。常为斑岩纹理。岩石学中,常见为辉绿岩(粗玄岩)。[1][2]
参见编辑
参考文献编辑
- ^ Examples of rocks with different names. [12 June 2015]. (原始内容存档于2020-05-06).
- ^ Igneous rock types - Australian Museum. [14 June 2015]. (原始内容存档于2015-06-03).
- Glazner, A. F., Bartley, J. M., Coleman, D. S., Gray, W. and Taylor, R. Z. (2004). "Are plutons assembled over millions of years by amalgamation from small magma chambers?" GSA Today, 14 (4: April), pp. 4–11.
- Young, Davis A. (2003). Mind Over Magma: the Story of Igneous Petrology. Princeton University Press. ISBN 0-691-10279-1.
- Best, Myron G. (1982). Igneous and Metamorphic Petrology. San Francisco: W. H. Freeman & Company. pp. 119 ff. ISBN 0-7167-1335-7.
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