ENSIKLOPEDIA Cari Tekan Enter untuk memulai pencarian cepat. Kembali ke Ensiklopedia Arsip Wikipedia Indonesia Anorogenic magmatism Anorogenic magmatismGeologic mechanism In geology, anorogenic magmatism is the formation, intrusion or eruption of magmas not directly connected with orogeny (mountain building).[1] Anorogenic magmatism occurs, for example, at mid-ocean ridges, hotspots and continental rifts. This contrasts with orogenic magmatism that occurs at convergent plate boundaries where continental collision, subduction and orogeny are common.[2] References ↑ Sheppard, S.M.F. (1986). "Chapter 10 – Igneous Rocks III – Isotopic Case Studies of Magmatism in Africa, Eurasia and Oceanic Islands". In Valley, J.W; Taylor, H.P.; O'Neil, J.R. (eds.). Stable Isoptopes in High Temperature Geological Processes (Reviews in Mineralogy – Volume 16). Mineralogical Society of America. p. 319. ISBN 0-939950-20-0. ↑ Anorogenic magmatism in Dronning Maud Land (Antarctica) vteMagmatic processesComponents of magma Liquid phase Igneous rocks Dissolved and exolved gases Processes Fractional crystallization Assimilation Magma mixing Magma mingling Exsolution of gases Outgassing Partial melting Anorogenic magmatism Flux melting Surface manifestations Igneous rock Geothermal systems Geothermal gradient anomalies Volcanism This article about igneous petrology is a stub. You can help Wikipedia by adding missing information.vte
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