Anomalous patterns of clay minerals in fault zones

XU Zhenhao, YU Tengfei, LIN Peng, LI Shucai - Engineering Geology, 2023 - Elsevier
The anomalous enrichment of clay minerals in fault zones is considered a key factor
affecting the seismic behavior of faults, fault permeability, and mineralization. This process …

Meteoric fluid infiltration in crustal-scale normal fault systems as indicated by δ18O and δ2H geochemistry and 40Ar/39Ar dating of neoformed clays in brittle fault …

S Haines, E Lynch, A Mulch, JW Valley… - …, 2016 - pubs.geoscienceworld.org
Both the sources and pathways of fluid circulation are key factors to understanding the
evolution of low-angle normal fault (LANF) systems and the distribution of mineral deposits …

Temperature micro-map** in oscillatory-zoned chlorite: Application to study of a green-schist facies fault zone in the Pyrenean Axial Zone (Spain)

V Trincal, P Lanari, M Buatier, B Lacroix… - American …, 2015 - degruyter.com
Oscillatory compositional zoning in minerals has been observed in hydrothermal, magmatic,
and metamorphic environments and is commonly attributed to chemical or physical cyclical …

Structure of lamprophyres: A discriminant marker for Variscan and Alpine tectonics in the Argentera-Mercantour Massif, Maritime Alps

M Filippi, D Zanoni, G Gosso… - Bulletin de la …, 2019 - pubs.geoscienceworld.org
Structural and microstructural analyses are carried out in two sites of the Argentera-
Mercantour Massif, Valscura and Val du Haut Boréon, where swarms of lamprophyres …

Fluid flow and polymetallic sulfide mineralization in the Kettara shear zone (Jebilet Massif, Variscan Belt, Morocco)

I N'diaye, A Essaifi, M Dubois, B Lacroix… - Journal of African Earth …, 2016 - Elsevier
The Kettara shear zone is a regional wrench shear zone within the Jebilet massif of Western
Morocco, part of the Variscan orogenic belt. This massif is characterized by bimodal …

Evidence of Tethyan continental break-up and Alpine collision in the Argentera-Mercantour Massif, Western Alps

M Filippi, D Zanoni, JM Lardeaux, MI Spalla, G Gosso - Lithos, 2020 - Elsevier
Abstract In the Argentera-Mercantour Massif, swarms of high-K calc-alkaline lamprophyres
intruded into Carboniferous migmatites and early Permian granites, likely in Permian …

A parametric analysis of fault reactivation in the New Madrid Seismic Zone: The role of pore fluid overpressure

H Leclère, É Calais - Journal of Geophysical Research: Solid …, 2019 - Wiley Online Library
Abstract Earthquakes in Stable Continental Regions (SCR), where localized present‐day
tectonic loading is negligible, remain difficult to explain. The New Madrid Seismic Zone …

[HTML][HTML] Worldwide shale-oil reserves: towards a global approach based on the principles of Petroleum System and the Petroleum System Yield

M Blaizot - Bulletin de la Société géologique de France, 2017 - pubs.geoscienceworld.org
Global inventory of shale-oil resources and reserves are far from being complete even in
mature basins which have been intensively drilled and produced and in which the main …

The spin zone: Transient mid-crust permeability caused by coseismic brecciation

BL Melosh, CD Rowe, C Gerbi, CE Bate… - Journal of Structural …, 2016 - Elsevier
Pore fluids migrating through the deep section of continental strike-slip fault zones have
been invoked to explain such phenomena as tectonic tremor, stress transfer across the …

[BOOK][B] Earthquake cycling in the brittle-plastic transition of a transform boundary: The Pofadder Shear Zone, Namibia and South Africa

BL Melosh - 2015 - search.proquest.com
Strain localization in ancient shear zones is critical to our understanding of earthquake cycle
processes at modern plate boundaries. The northwest-southeast oriented, dextral, Pofadder …