词条 | Deep hot zone |
释义 |
In geology, a deep hot zone refers to the process where a number of mafic sills intrude into the "moho", the region between the Earth's crust and the mantle.[1] References1. ^{{cite journal|first1=Catherine |last1=Annen|first2=Jonathan D. |last2=Blundy |first3=R. Stephen J. |last3=Sparks|date=1 August 2008|title=The sources of granitic melt in Deep Hot Zones|journal=Earth and Environmental Science Transactions of the Royal Society of Edinburgh|publisher=The Royal Society of Edinburgh|volume=97|issue=4|pages=297–309|oclc=316058546|url=https://www.cambridge.org/core/journals/earth-and-environmental-science-transactions-of-royal-society-of-edinburgh/article/sources-of-granitic-melt-in-deep-hot-zones/F1F69A138A3CC3BD47D5329F403285AE|accessdate=18 December 2017}} {{geology-stub}} 1 : Geology terminology |
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