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زبان محتوا

پشتیبانی: CRM@email.irandoc.ac.ir

Concept information

اصطلاح مرجح

مجموعه فرورانشی فرابالا  

نوع

  • http://www.irandoc.ac.ir/onto/irandoc-meta/Concept

تعاریف

  • There is increasing evidence that most ophiolites are generated when subduction begins and thus represent fragments of fore-arc lithosphere. This led to introduction of the term ‘supra-subduction zone’ (SSZ) ophiolite in the 1980s to acknowledge that some ophiolites are more closely related to island arcs than ocean ridges. [Wikipedia]

منسوخ

  • false

در زبان های دیگر

URI

http://www.irandoc.acir/onto/irandoc/SWEETT00930

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