Search Results - "Zandomeneghi, D."

Texture analysis of volcanic rock samples: Quantitative study of crystals and vesicles shape preferred orientation from X-ray microtomography data by Voltolini, M., Zandomeneghi, D., Mancini, L., Polacci, M.

“…In the texture analysis of volcanic rocks, the preferred orientation of the constituents can provide useful information for the interpretation of the processes…”
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Internal structure of Erebus volcano, Antarctica imaged by high-resolution active-source seismic tomography and coda interferometry by Zandomeneghi, D., Aster, R., Kyle, P., Barclay, A., Chaput, J., Knox, H.

“…Erebus volcano, Antarctica has hosted a persistent convecting phonolite lava lake for over 40 years. The lake produces small (VEI 0–1) Strombolian eruptions…”
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Imaging of Erebus volcano using body wave seismic interferometry of Strombolian eruption coda by Chaput, J. A., Zandomeneghi, D., Aster, R. C., Knox, H., Kyle, P. R.

“…Seismic interferometry is a recently developed theory that allows for the recovery of a medium's impulse response between two points should randomly…”
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Analysis of dynamics of vulcanian activity of Ubinas volcano, using multicomponent seismic antennas by Inza, L.A., Métaxian, J.P., Mars, J.I., Bean, C.J., O'Brien, G.S., Macedo, O., Zandomeneghi, D.

“…A series of 16 vulcanian explosions occurred at Ubinas volcano between May 24 and June 14, 2009. The intervals between explosions were from 2.1h to more than…”
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Moment tensor inversion of very long period seismic signals from Strombolian eruptions of Erebus Volcano by Aster, R., Zandomeneghi, D., Mah, S., McNamara, S., Henderson, D.B., Knox, H., Jones, K.

“…Strombolian eruptions from the long-lived lava lake of Erebus volcano, Ross Island, Antarctica, generate repeating Very Long Period (VLP) signals, containing…”
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Role of conduit shear on ascent of the crystal-rich magma feeding the 800-year-B.P. plinian eruption of Quilotoa volcano (Ecuador) by ROSI, M, LANDI, P, POLACCI, M, DI MURO, A, ZANDOMENEGHI, D

“…We have characterized pumice products belonging to the climactic phase of the 800-year-b.p. Quilotoa eruption. Bulk rock compositions, petrography, mineral,…”
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