DC Bradley - Earth-Science Reviews, 2008 - Elsevier
Passive margins have existed somewhere on Earth almost continually since 2740 Ma. They were abundant at 1900–1890, 610–520, and 150–0 Ma, scarce at ca. 2445–2300, 1600 …
IGNEOUS ROCKS AND PROCESSES A practical introduction to igneous petrology for students and practitioners The newly revised Second Edition of Igneous Rocks and …
The Eastern Mediterranean region exhibits a fascinating diversity of ophiolites and related oceanic magmatic units of mainly Triassic, Jurassic and Cretaceous age. Comparisons with …
Suprasubduction zone (SSZ) ophiolites display a consistent sequence of events during their formation and evolution that suggests that they form in response to processes that are …
This paper presents new ideas on the Early Palaeozoic geography and tectonic history of the Iapetus Ocean involved in the formation of the northern Appalachian-British Caledonide …
W Springer, HA Seck - Contributions to Mineralogy and Petrology, 1997 - Springer
Partial fusion experiments with basic granulites (S6, S37) believed to represent the lower crust beneath the Eifel region (Germany) were performed at pressures from 5 to 15 kbar …
The most commonly used tectonic discrimination diagrams for granites were introduced by Pearce et al.[Pearce, JA, Harris, NBW, Tindle, AG, 1984. Trace element discrimination …
J Berndt, J KOEPKE, F Holtz - Journal of Petrology, 2005 - academic.oup.com
Crystallization experiments were performed at 200 MPa in the temperature range 1150– 950° C at oxygen fugacities corresponding to the quartz–fayalite–magnetite (QFM) and MnO …
J Wakabayashi, Y Dilek - Geological Society, London, Special …, 2003 - lyellcollection.org
Ophiolites have long been recognized as on-land fragments of fossil oceanic lithosphere, which becomes an ophiolite when incorporated into continental margins through a complex …