Trace element geochemistry of epidote minerals

D Frei, A Liebscher, G Franz… - Reviews in Mineralogy …, 2004 - pubs.geoscienceworld.org
One of the most striking features of epidote minerals is their ability to incorporate significant
amounts of geochemically important trace elements such as large ion lithophile elements …

Combined thermodynamic–geochemical modeling in metamorphic geology: boron as tracer of fluid–rock interaction

M Konrad-Schmolke, R Halama - Lithos, 2014 - Elsevier
Quantitative geochemical modeling is today applied in a variety of geological environments
from the petrogenesis of igneous rocks to radioactive waste disposal. In addition, the …

Aqueous fluids and hydrous melts in high-pressure and ultra-high pressure rocks: implications for element transfer in subduction zones

J Hermann, C Spandler, A Hack, AV Korsakov - Lithos, 2006 - Elsevier
High-pressure (HP) and ultra-high pressure (UHP) terranes are excellent natural
laboratories to study subduction-zone processes. In this paper we give a brief theoretical …

Metamorphic chemical geodynamics of subduction zones

GE Bebout - Earth and Planetary Science Letters, 2007 - Elsevier
Study of metamorphic suites directly representing the deep subduction of altered oceanic
crust and sediments can help elucidate the geochemical evolution of the forearc-to-subarc …

Trace element fractionation during fluid-induced eclogitization in a subducting slab: trace element and Lu–Hf–Sm–Nd isotope systematics

T John, EE Scherer, K Haase, V Schenk - Earth and Planetary Science …, 2004 - Elsevier
Spatially closely associated gabbros and eclogites of central Zambia represent relics of
subducted oceanic crust in a suture zone. The eclogites, which formed at 630–690° C and …

Cycling of B, Li, and LILE (K, Cs, Rb, Ba, Sr) into subduction zones: SIMS evidence from micas in high-P/T metasedimentary rocks

GE Bebout, AE Bebout, CM Graham - Chemical Geology, 2007 - Elsevier
The Catalina Schist (California) affords a unique opportunity to evaluate the effects of
varying prograde P–T paths on the magnitudes of devolatilization and chemical/isotopic …

Fluid–rock interaction and element mobilization in UHP metabasalt: constraints from an omphacite–epidote vein and host eclogites in the Dabie orogen

S Guo, K Ye, Y Chen, J Liu, Q Mao, Y Ma - Lithos, 2012 - Elsevier
A petrological study is carried out for a high-pressure (HP) omphacite–epidote vein and its
host ultrahigh-pressure (UHP) eclogites at Ganghe in the Dabie orogen. The UHP eclogite …

Petrology of HP metamorphic veins in coesite-bearing eclogite from western Tianshan, China: fluid processes and elemental mobility during exhumation in a cold …

Z Lü, L Zhang, J Du, X Yang, Z Tian, B Xia - Lithos, 2012 - Elsevier
A petrological study was carried out for high pressure (HP) veins which cut through the host
coesite-bearing eclogites at Habutengsu–Kebuerte in western Tianshan, China. The results …

New occurrence of UHP eclogites in Limousin (French Massif Central): age, tectonic setting and fluid–rock interactions

J Berger, O Féménias, D Ohnenstetter, O Bruguier… - Lithos, 2010 - Elsevier
Kyanite and zoisite eclogites from the Limousin area in the Variscan French Massif Central
(FMC) have been formed by deep subduction to 100km depth at peak pressure–temperature …

Reaction rind formation in the Catalina Schist: Deciphering a history of mechanical mixing and metasomatic alteration

SC Penniston-Dorland, JK Gorman, GE Bebout… - Chemical …, 2014 - Elsevier
In the subduction-related Catalina Schist, reaction zones or 'rinds' developed at contacts of
metamorphosed mafic blocks with chemically distinct mélange matrix. These rinds exhibit …