Results 61 to 70 of about 74,121 (304)

Notable Impact of Paleotectonic Stress on Gold Mineralisation in the West Qinling Orogen

Geological Journal, EarlyView.
By applying fuzzy clustering and multiple inverse methods, we systematically processed the data of vein and fault slip in this ore deposit to reveal the transition of orogenic geological environment and paleotectonic stress field. Our research results show two different stress states: the northwest–southeast extensional stress field and the northeast ...
Hongyan Wang, Aibing Chen, Jian Yang, Yuan Zhang   +3 more
wiley   +1 more source

Investigating Global Correlations Between Earthquake-generated Tsunamis and Subduction Zone Characteristics

Tektonika
Tsunamigenic earthquakes pose a large hazard in subduction zones, but it is currently unclear in which - if any - tectonic setting they preferentially occur.
Iris van Zelst, Silvia Brizzi, Elenora van Rijsingen, Francesca Funiciello , Ylona van Dinther   +4 more
doaj   +1 more source

Earthquake slip surfaces identified by biomarker thermal maturity within the 2011 Tohoku-Oki earthquake fault zone. [PDF]

, 2020
Extreme slip at shallow depths on subduction zone faults is a primary contributor to tsunami generation by earthquakes. Improving earthquake and tsunami risk assessment requires understanding the material and structural conditions that favor earthquake ...
Kirkpatrick, James D, Polissar, Pratigya J, Rabinowitz, Hannah S, Rowe, Christie D, Savage, Heather M   +4 more
core  

Tertiary-Quaternary subduction processes and related magmatism in the Alpine-Mediterranean region [PDF]

, 2006
During Tertiary to Quaternary times, convergence between Eurasia and Africa resulted in a variety of collisional orogens and different styles of subduction in the Alpine-Mediterranean region.
Downes, Hilary, Harangi, Szabolcs, Seghedi, I.   +2 more
core   +1 more source

Geochemical and Geological Investigation of Skarn‐Type Pb–Zn Mineralization in Hastanetepe (Balya‐Balıkesir, Türkiye): An Approach Based on Fluid Inclusions, Sulphur Isotopes and Geochemical Data

Geological Journal, EarlyView.
Integrated petrographic, mineralogical and geochemical data from the Hastanetepe Pb–Zn deposit (Balya, Türkiye) reveal multi‐stage hydrothermal alteration and a magmatic sulphur source. Fluid inclusion and sulphur isotope results indicate a complex fluid evolution responsible for skarn‐type Pb–Zn mineralization along limestone–dacite contacts ...
Esra Ünal‐Çakır
wiley   +1 more source

Horizontally forced initiation of the Izu-Bonin-Mariana subduction zone

Communications Earth & Environment
The sparsity of a direct record for the moment of subduction zone initiation has led to various models describing the infancy and evolution of modern oceanic subduction systems.
Liang Liu, Hong-Yan Li, Lijun Liu, Jeffrey G. Ryan, Jason P. Morgan, Ke-Xin Ren, Yi-Gang Xu   +6 more
doaj   +1 more source

Two-sided asymmetric subduction; implications for tectonomagmatic and metallogenic evolution of the Lut Block, Eastern Iran [PDF]

, 2011
West directed subduction zones show common characteristics, such as low structural elevation, deep trench, steep slab and a conjugate back-arc basin that are opposite to those of the east directed subduction zones.
Arjmandzadeh, R., Homam, S. M., Karimpour, M. H., Mazaheri, S. A., Medina, J. M., Santos, J. F.   +5 more
core   +2 more sources

Interseismic coupling and seismic potential along the Central Andes subduction zone [PDF]

, 2011
We use about two decades of geodetic measurements to characterize interseismic strain build up along the Central Andes subduction zone from Lima, Peru, to Antofagasta, Chile.
Aktug, Altamimi, Altamimi, Altamimi, Arriagada, Arriagada, Arriagada, Arriagada, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Baby, Baby, Baby, Baby, Baby, Baby, Baby, Baby, Barke, Barke, Barke, Barrientos, Barrientos, Barrientos, Bassin, Bassin, Bassin, Beck, Beck, Beck, Beck, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Biggs, Biggs, Biggs, Bilek, Bilek, Brown, Brown, Brown, Brown, Béjar-Pizarro, Bürgmann, Bürgmann, Bürgmann, Bürgmann, Bürgmann, Bürgmann, Chen, Chen, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Collot, Collot, Collot, Collot, Collot, Collot, Collot, Collot, Collot, Comte, Comte, Comte, Comte, Comte, Comte, Comte, Delouis, Delouis, Delouis, Delouis, DeMets, DeMets, DeMets, DeMets, Dominique Remy, Dorbath, Dorbath, Dorbath, Dragert, Dragert, Dragert, Engdhal, Engdhal, Engdhal, Farr, Farr, Francis Bondoux, Freymueller, Freymueller, Freymueller, Frédérique Rolandone, Gagnon, Gagnon, Gagnon, Germinal Gabalda, Giovanni, Giovanni, Giovanni, Hashimoto, Hashimoto, Hashimoto, Hashimoto, Haskell, Heki, Heki, Hernando Tavera, Hetland, Hetland, Hetland, Hindle, Hindle, Hindle, Hindle, Hindle, Hindle, Hirose, Hirose, Hirose, Hirose, Hirose, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hu, Hu, Hu, Hu, Hu, Hugo Perfettini, Hyndman, Hyndman, Hyndman, Jean-Mathieu Nocquet, Jean-Philippe Avouac, Ji, Ji, Ji, Johnson, Johnson, Kanamori, Kanamori, Kanda, Kanda, Kaneko, Kaneko, Kaneko, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Kley, Kley, Konca, Lamb, Langer, Langer, Liu, Liu, Llenos, Llenos, Loveless, Loveless, Loveless, Loveless, Loveless, Loveless, Loveless, Lowry, Lowry, Lowry, Lowry, Massonnet, Massonnet, Massonnet, Massonnet, Massonnet, Massonnet, Massonnet, McQuarrie, McQuarrie, McQuarrie, Melnick, Melnick, Melnick, Melnick, Miyazaki, Miyazaki, Miyazaki, Mohamed Chlieh, Moreno, Moreno, Moreno, Motagh, Motagh, Motagh, Motagh, Motagh, Motagh, Motagh, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Oleskevich, Oleskevich, Oleskevich, Oncken, Oncken, Oncken, Oncken, Oncken, Oncken, Oncken, Perfettini, Perfettini, Perfettini, Perfettini, Perfettini, Perfettini, Perfettini, Peyrat, Peyrat, Peyrat, Peyrat, Peyrat, Peyrat, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Robinson, Robinson, Robinson, Salichon, Salichon, Salichon, Salichon, Salichon, Salichon, Savage, Scholz, Sella, Sella, Sella, Silgado, Simons, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Song, Song, Spence, Spence, Spence, Spence, Spence, Swenson, Swenson, Sylvain Bonvalot, Tavera, Tavera, Tavera, Tavera, Tavera, Tavera, Tavera, Thatcher, Tichelaar, Tichelaar, Vergne, Vergne, Vergne, Victor, Victor, Victor, Victor, Victor, Vigny, Vigny, Vigny, Vigny, Vigny, Vigny, Walker, Wallace, Wallace, Wallace, Wallace, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wells, Wells, Wells, Wells, Wells, Xie, Xie, Yoshioka, Yoshioka, Yoshioka, Yoshioka, Yoshioka, Yoshioka   +380 more
core   +5 more sources

Response of Remote Tropical West Pacific Islands to Climate Variability: A Multiproxy Record From T‐Lake, Palau, Spanning the Early Holocene to Present

Archaeometry, EarlyView.
ABSTRACT Lake sediments are natural archives of past environmental dynamics and how these systems have responded to past climate variability. Sediment geochemistry, governed by local geology and climate processes, is unique to each lake‐catchment and geochemical proxies must be validated for each study site.
Jalene Nalbant, Larissa Schneider, Jessica L. Blois, Matthew Wolhowe, Julian P. Sachs, Simon G. Haberle, Geoffrey Clark   +6 more
wiley   +1 more source

On the fluid-mobility of molybdenum, tungsten, and antimony in subduction systems [PDF]

, 2011
Molybdenum (Mo) and tungsten (W) have long been regarded as being more or less immobile during slab fluid-induced arc magma generation. Here we characterize about 180 samples of young, predominantly mafic to intermediate tephras and lavas for their Mo,
Garbe-Schönberg, Dieter, Halama, Ralf, Heydolph, Ken, Hoernle, Kaj, Jacques, Guillaume, Mahlke, Julia, Schumann, Kai, Wehrmann, Heidi   +7 more
core