scholarly journals Tephra glass chemistry provides storage and discharge details of five magma reservoirs which fed the 75 ka Youngest Toba Tuff eruption, northern Sumatra

2019 ◽  
Vol 35 (1-2) ◽  
pp. 256-271 ◽  
Author(s):  
Nicholas J.G. Pearce ◽  
John A. Westgate ◽  
Guilherme A.R. Gualda ◽  
Emma Gatti ◽  
Ros F. Muhammad
Keyword(s):  
Magma Reservoirs ◽  
Glass Chemistry

DIFFUSION CHRONOMETRY IN SANIDINE: HELPING UNRAVEL THERMAL HISTORIES OF LARGE SILICIC MAGMA RESERVOIRS

2019 ◽  
Author(s):  
Jordan Lubbers ◽  
◽  
Adam J.R. Kent ◽  
Frank Tepley ◽  
Dawid Szymanowski
Keyword(s):  
Silicic Magma ◽  
Diffusion Chronometry ◽  
Magma Reservoirs ◽  
Thermal Histories

scholarly journals Glass Chemistry to Analyze Human Cells under Adverse Conditions

ACS Omega ◽  
2019 ◽  
Vol 4 (7) ◽  
pp. 11515-11521 ◽  
Author(s):  
Angela N. Marquard ◽  
Jonathan C. T. Carlson ◽  
Ralph Weissleder
Keyword(s):  
Human Cells ◽  
Adverse Conditions ◽  
Glass Chemistry

Lineaments Revisited

SEG Discovery ◽  
2000 ◽  
pp. 1-20
Author(s):  
JEREMY P. RICHARDS
Keyword(s):  
Large Scale ◽  
Mineral Exploration ◽  
Porphyry Copper ◽  
Regional Scale ◽  
Tectonic Events ◽  
Magma Reservoirs ◽  
Magma Supply ◽  
Magmatic History ◽  
Lithospheric Stress ◽  
Crustal Magma

ABSTRACT Large-scale crustal lineaments are recognized as corridors (up to 30 km wide) of aligned geological, structural, geomorphological, or geophysical features that are distinct from regional geological trends such as outcrop traces. They are commonly difficult to observe on the ground, the scale of the features and their interrelationships being too large to map except at a regional scale. They are therefore most easily identified from satellite imagery and geophysical (gravity, magnetic) maps. Lineaments are believed to be the surface expressions of ancient, deep-crustal or trans-lithospheric structures, which periodically have been reactivated as planes of weakness during subsequent tectonic events. These planes of weakness, and in particular their intersections, may provide high-permeability channels for ascent of deeply derived magmas and fluids. Optimum conditions for magma penetration are provided when these structures are placed under tension or transtension. In regions of subduction-related magmatism, porphyry copper and related deposits may be generated along these lineaments because the structures serve to focus the ascent of relatively evolved magmas and fluid distillates from deep-crustal magma reservoirs. However, lineament intersections can only focus such activity where a magma supply exists, and when lithospheric stress conditions permit. A comprehensive understanding of regional tectono-magmatic history is therefore required to interpret lineament maps in terms of their prospectivity for mineral exploration.

Locating magma reservoirs using InSAR and petrology before and during the 2011–2012 Cordón Caulle silicic eruption

2014 ◽  
Vol 395 ◽  
pp. 254-266 ◽  
Author(s):  
Jennifer Jay ◽  
Fidel Costa ◽  
Matthew Pritchard ◽  
Luis Lara ◽  
Bradley Singer ◽  
...  
Keyword(s):  
Magma Reservoirs

scholarly journals Exsolved volatiles in magma reservoirs

2018 ◽  
Vol 368 ◽  
pp. 13-30 ◽  
Author(s):  
Marie Edmonds ◽  
Andrew W. Woods
Keyword(s):  
Magma Reservoirs

scholarly journals Integrated magnetotelluric and petrological analysis of felsic magma reservoirs: Insights from Ethiopian rift volcanoes

2021 ◽  
Author(s):  
Friedemann Samrock ◽  
Alexander Grayver ◽  
Olivier Bachmann ◽  
Özge Karakas ◽  
Martin Saar
Keyword(s):  
Ethiopian Rift ◽  
Felsic Magma ◽  
Magma Reservoirs
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