Results 91 to 100 of about 2,053 (253)
Physical processes in volcanic eruptions.
Volcanoes can be regarded as probes of the composition and structure of a planetary interior as a function of position, depth and time.
Wilson, L., Pinkerton, H., Macdonald, R.
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Abstract The seismic behavior of subduction megathrusts varies spatially and is influenced by the properties of subducting plates, including their sedimentary cover. Characterizing these subduction inputs is essential for understanding the mechanisms behind fault slip variability.
Philip M. Barnes +12 more
wiley +1 more source
Fundamentals of physical volcanology
Fundamentals of Physical Volcanology is a comprehensive overview of the processes that control when and how volcanoes erupt. Understanding these processes involves bringing together ideas from a number of disciplines, including branches of geology, such ...
Parfitt, Elizabeth A.
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Volcanic History and Eruption Processes of Blue Lake Crater, Tongariro
Blue Lake Crater (BLC) is a volcanic crater lake situated on the northern end of the Tongariro Volcanic Centre (TgVC) and is one of at least 11 vents that have been active since c. 25 ka.
Simons, Benjamin Clifford
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Why LA‐ICPMS Fission‐Track Age Data Are So Dispersed? A Pseudo‐EDM Solution
Abstract Fission track (FT) dating is a well‐established thermochronological technique widely used to reconstruct rocks' thermal histories. Over the past two decades, development of Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA‐ICPMS) has significantly advanced the application of FT dating by enabling rapid measurements of uranium ...
Yuntao Tian, Huixia Zhong
wiley +1 more source
Easily updatable information on ecosystem condition (EC) is essential for understanding trends in ecosystem degradation and prioritising restoration efforts.
Isabel Nicholson Thomas +19 more
doaj +1 more source
Grain Size and Fluid Effects on the Frictional Behavior of Simulated Carbonate Fault Gouge
Abstract Carbonate rocks exhibit a span of clast and grain size in fault zones. However, the effect of grain size distribution on the frictional behavior of carbonate faults and its implications for natural and induced seismicity remain poorly understood.
Entela Kane +2 more
wiley +1 more source
Transient Porosity During Fluid‐Mineral Interaction. Part 1: In Situ 4D Tomography
Abstract Fluid‐induced mineral replacement reactions play a key role in controlling porosity generation and permeability evolution in geologic systems. However, the dynamic feedback between pore structure development and fluid transport remains poorly quantified. This study investigates the spatiotemporal evolution of reaction‐induced pore space in the
Hamed Amiri +7 more
wiley +1 more source
A Thesis submitted to the faculty of the Graduate School of the University of Minnesota by Jan Albert de Beer in partial fulfillment of the requirements for the degree of Master of Science, October 1997.This thesis represents the results of a geologic ...
de Beer, Jan Albert
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Transient Porosity During Fluid‐Mineral Interaction, Part 2: Reconstruction Using Generative AI
Abstract Quantifying fluid–rock interactions within the lithosphere is vital for both geological processes and applications such as CO2 ${\text{CO}}_{2}$ storage and geothermal energy development. Mineral replacement reactions generate transient pore networks that enhance fluid flow, yet many pores become isolated once reactions are completed, reducing
Hamed Amiri +5 more
wiley +1 more source

