Eclogitization of glaucophanites by fluid infiltration

2000 ◽  
Vol 43 (S1) ◽  
pp. 144-155 ◽  
Author(s):  
Jun Gao ◽  
R. Klemd ◽  
Shengwei Liu
Keyword(s):  
Fluid Infiltration

Evaluating drilling fluid infiltration in porous media – Comparing NMR, gravimetric, and X-ray CT scan methods

2021 ◽  
Vol 198 ◽  
pp. 108242
Author(s):  
Badr S. Bageri ◽  
Abdulrauf R. Adebayo ◽  
Jaber Al Jaberi ◽  
Shirish Patil ◽  
Rahul B. Salin
Keyword(s):  
Porous Media ◽  
Ct Scan ◽  
Drilling Fluid ◽  
X Ray ◽  
Fluid Infiltration

scholarly journals Meteoric fluid infiltration in crustal-scale normal fault systems as indicated by δ18O and δ2H geochemistry and40Ar/39Ar dating of neoformed clays in brittle fault rocks

Lithosphere ◽  
2016 ◽  
Vol 8 (6) ◽  
pp. 587-600 ◽  
Author(s):  
Samuel Haines ◽  
Erin Lynch ◽  
Andreas Mulch ◽  
John W. Valley ◽  
Ben van der Pluijm
Keyword(s):  
Normal Fault ◽  
Fault Rocks ◽  
Fault Systems ◽  
Fluid Infiltration

Fluid Infiltration Through Oceanic Lower Crust in Response to Reaction‐Induced Fracturing: Insights From Serpentinized Troctolite and Numerical Models

2020 ◽  
Vol 125 (11) ◽  
Author(s):  
Kazuki Yoshida ◽  
Atsushi Okamoto ◽  
Hiroyuki Shimizu ◽  
Ryosuke Oyanagi ◽  
Noriyoshi Tsuchiya ◽  
...  
Keyword(s):  
Lower Crust ◽  
Numerical Models ◽  
Fluid Infiltration

scholarly journals Eocene and Miocene extension, meteoric fluid infiltration, and core complex formation in the Great Basin (Raft River Mountains, Utah)

Tectonics ◽  
2015 ◽  
Vol 34 (4) ◽  
pp. 680-693 ◽  
Author(s):  
Katharina Methner ◽  
Andreas Mulch ◽  
Christian Teyssier ◽  
Michael L. Wells ◽  
Michael A. Cosca ◽  
...  
Keyword(s):  
Complex Formation ◽  
Great Basin ◽  
Core Complex ◽  
Fluid Infiltration

scholarly journals Exotic garnet–clinopyroxene–K-feldspar granulites from the Chepelare shear zone, Central Rhodope massif, Bulgaria: implications for high-pressure granulite facies metamorphism

2019 ◽  
Vol 48 (3) ◽  
pp. 49-63
Author(s):  
Milena Georgirva ◽  
Tzvetomila Vladinova
Keyword(s):  
Shear Zone ◽  
Thick Layer ◽  
Granulite Facies ◽  
Mineral Association ◽  
Granulite Facies Metamorphism ◽  
Fine Grain ◽  
Fluid Infiltration ◽  
High Pressure Granulite ◽  
The Matrix ◽  
Homogeneous Matrix

Garnet–clinopyroxene–K-feldspar granulite occurs as a thick layer or boudin within the variegated rocks of the Chepelare shear zone in the Central Rhodope massif, Bulgaria. It consists of several domains: mesocratic homogeneous matrix (clinopyroxene–plagioclase–K-feldspar–quartz ± amphibole), porphyroblastic garnet, K-feldspar and clinopyroxene, and strongly foliated fine-grain bands (chloritized biotite–chlorite–prehnite–albite ± epidote). The origin and nature of the matrix mineral association is still unclear. The peak porphyroblast association forms at the expense of plagioclase from the matrix at higher pressure. The fine-grain deformation zones channel the lattermost fluid infiltration. The clinopyroxene-garnet and Zr-in-titanite thermometry give temperatures higher than 790–860 ºC at 2 GPa and, with thermodynamic modeling, suggests crystallization at ~1.8–2.1 GPa and temperature of ~850 ºC in HP granulite field for the porphyroblast granulite association.

Hemodynamic Changes and Fluid Shifts After Large-Volume Fluid Infiltration

2010 ◽  
Vol 64 (1) ◽  
pp. 83-88 ◽  
Author(s):  
Selahattin Ozmen ◽  
Krzysztof Kusza ◽  
Betul G. Ulusal ◽  
Landon Pryor ◽  
Maria Siemionow ◽  
...  
Keyword(s):  
Large Volume ◽  
Hemodynamic Changes ◽  
Fluid Infiltration ◽  
Fluid Shifts

Synorogenic crustal fluid infiltration in the Idaho-Montana Thrust Belt

2001 ◽  
Vol 28 (22) ◽  
pp. 4295-4298 ◽  
Author(s):  
Gray E. Bebout ◽  
David J. Anastasio ◽  
James E. Holl
Keyword(s):  
Thrust Belt ◽  
Crustal Fluid ◽  
Fluid Infiltration
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