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Article . 1996 . Peer-reviewed
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Ultrahigh Pressure Metamorphism: Cambridge Topics in Petrology

descriptionPublicationkeyboard_double_arrow_right Article 06 Aug 1996Publisher:American Geophysical Union (AGU)Journal:Eos, Transactions American Geophysical Union, volume 77, pages 310-310 (issn: 0096-3941, eissn: 2324-9250, Copyright policy )
Authors: Bernard W. Evans;

doi: 10.1029/96eo00221

Ultrahigh Pressure Metamorphism: Cambridge Topics in Petrology

Abstract

The field of ultra‐high pressure metamorphism (UHPM) emerged only 12 years ago when microscopic relics of coesite were found in crustal rocks that had been metamorphosed during subduction related to continental collision. Coesite‐bearing metamorphic rocks were soon found elsewhere, and then metamorphic microdiamonds were discovered. Suddenly, the pressure axis for orogenic metamorphism had expanded from 1.5–2.0 to 3.0–4.0 GPa!

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citations
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
2
Average
Average
Average
gold