نتایج جستجو برای: pyroclastic units

تعداد نتایج: 172732  

2017
H. H. Schmitt

Integration of Apollo 17 field observations and photographs, sample investigations, Lunar Reconnaissance Orbiter Camera images, Chandrayaan-1 Moon Mineralogy Mapper (M 3 ) spectra, and Miniature Radio Frequency (Mini-RF) S-band radar images provides new insights into the geology of the valley of Taurus– Littrow on the Moon. Connecting the various remote observations to sample data enables a set...

2014
Bruce A. Campbell B. Ray Hawke Gareth A. Morgan Lynn M. Carter Donald B. Campbell Michael Nolan

Radar images at 70 cm wavelength show 4–5 dB variations in backscatter strength within regions of relatively uniform spectral reflectance properties in central and northern Mare Serenitatis, delineating features suggesting lava flow margins, channels, and superposition relationships. These backscatter differences are much less pronounced at 12.6 cmwavelength, consistent with a large component o...

2007
J. Dufek M. Manga M. Staedter

[1] Steam explosions, or littoral blasts, generated when pyroclastic flows interact with seawater may be a common, although rarely documented, phenomena. The development of steam explosions rather than passive steam production is related to the rate of thermal energy transfer from hot pyroclasts to water. We conduct a series of laboratory experiments to quantify the heat transfer and steam prod...

2009
Walter S. Kiefer

Introduction The Aristarchus Plateau (Figure 1) is a distinctive, geologically complex volcanic highland in northern Oceanus Procellarum. It is roughly diamond shaped, 170 by 220 km across, and up to 2 km higher than the surrounding mare [1, 2]. The roughly linear edges of the plateau suggest that it is fault bounded. The plateau edges are essentially radial and concentric to the center of the ...

Journal: :Occupational and environmental medicine 2002
D G Housley K A Bérubé T P Jones S Anderson F D Pooley R J Richards

BACKGROUND The Soufriere Hills, a stratovolcano on Montserrat, started erupting in July 1995, producing volcanic ash, both from dome collapse pyroclastic flows and phreatic explosions. The eruptions/ash resuspension result in high concentrations of suspended particulate matter in the atmosphere, which includes cristobalite, a mineral implicated in respiratory disorders. AIMS To conduct toxico...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2014
Marie D Jackson Eric N Landis Philip F Brune Massimo Vitti Heng Chen Qinfei Li Martin Kunz Hans-Rudolf Wenk Paulo J M Monteiro Anthony R Ingraffea

The pyroclastic aggregate concrete of Trajan's Markets (110 CE), now Museo Fori Imperiali in Rome, has absorbed energy from seismic ground shaking and long-term foundation settlement for nearly two millenia while remaining largely intact at the structural scale. The scientific basis of this exceptional service record is explored through computed tomography of fracture surfaces and synchroton X-...

2014
Teresa Scolamacchia Donald B. Dingwell

Understanding the mechanisms that govern ash aggregation is of critical importance in volcanology. Aggregation reduces the residence time of ash (≤2 mm) in the atmosphere strongly, by enhancing the sedimentation of finer-grained material generated during explosive eruptions. To date, experimental studies have focused on the expectation that water provides the strongest bonds between particles t...

2017
Christoph Schmidt Jean Pierre Tchouankoue Peguy Noel Nkouamen Nemzoue Félicité Ayaba Siggy Signe Nformidah-Ndah Emmanuel Nformi Chifu

Nyos maar is located in the Cameroon Volcanic Line and generates a multitude of primary and secondary hazards to the local population. For risk assessment and hazard mitigation, the age of the Nyos maar eruption provides some vital information. Since previous dating efforts using a range of techniques resulted in vastly varying eruption ages, we applied thermoluminescence (TL) methods to obtain...

ابراهیمی نصر آبادی, خسرو, حیدریان شهری, محمدرضا, شجاعی‌زاده اقدم, شیرین,

Estaj manganese deposit is located close to the Estaj village, 40 km southwest of Sabzevar, in Central Iran and Sabzevar subzone. Based on field evidences and microscopic studies, the rock units of the study area are pyroxene hornblende tracy Andesite, crystalin andesitic tuff, pyroxen hornblende andesite, pyroxen andesite- basalt, chert and limstone. These rock units belong to Late Cretaceous ...

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