A. T. Linde

Carnegie Institution for Science

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

S. I. Sacks

Japan Agency for Marine-Earth Science and Technology

I. Selwyn Sacks

Carnegie Institution for Science

B. Voight

Pennsylvania State University

P. E. Malin

Applied Spectral Imaging (United States)

G. S. Mattioli

The University of Texas at Arlington

D. Hidayat

Politeknik STMI Jakarta

E. Shalev

Duke University

M. J. S. Johnston

University of Sussex

Derek Elsworth

Pennsylvania State University

Alexandre Canitano

Institute of Earth Sciences, Academia Sinica

Cooperative Institutions

United States Geological Survey

Istituto Nazionale di Geofisica e Vulcanologia

Centre National de la Recherche Scientifique

Institut de physique du globe de Paris

Montserrat Volcano Observatory

Pennsylvania State University

Stanford University

Carnegie Institution for Science

University of Iceland

Menlo School

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Magma Chamber Recharging During Eruption and Tectonic Influence on Reservoirs: an Example From the 1986 Eruption of Izu-Oshima

AGU Fall Meeting Abstracts (2013)

A. T. Linde Osamu Kamigaichi Masaaki Churei Kenji Kanjo S. I. Sacks

Magma chamber

Phreatic eruption

Lateral eruption

Effusive eruption

Vulcanian eruption

Dense-rock equivalent

Peléan eruption

Source

Cite

Citations (0)

Source complexity of small earthquakes near Matsushiro, Japan

Tectonophysics (1989)

Jon P. Davis I. Selwyn Sacks A. T. Linde

Seismogram

Seismometer

Coda

Seismic moment

10.1016/0040-1951(89)90212-6

Cite

Citations (4)

Fault failure with moderate earthquakes

Tectonophysics (1987)

M. J. S. Johnston A. T. Linde M. T. Gladwin Roger D. Borcherdt

Moment magnitude scale

Fault plane

Seismic moment

Earthquake rupture

10.1016/0040-1951(87)90017-5

Cite

Citations (89)

Borehole observations of continuous strain and fluid pressure

Springer eBooks (2006)

Evelyn Roeloffs A. T. Linde

Strain (injury)

10.1007/978-3-540-49302-0_9

Cite

Citations (31)

Prototype PBO instrumentation of CALIPSO project captures world‐record lava dome collapse on Montserrat Volcano

Eos (2004)

G. S. Mattioli S. R. Young B. Voight R. Steven J. Sparks

This article is an update on the status of an innovative new project designed to enhance generally our understanding of andesitic volcano eruption dynamics and, specifically the monitoring and scientific infrastructure at the active Soufrière Hills Volcano (SHV), Montserrat. The project has been designated as the Caribbean Andesite Lava Island Precision Seismo‐geodetic Observatory known as CALIPSO. Its purpose is to investigate the dynamics of the entire SHV magmatic system using an integrated array of specialized instruments in four strategically located ∼200‐m‐deep boreholes in concert with several shallower holes and surface sites. The project is unique, as it represents the first, and only such borehole volcano‐monitoring array deployed at an andesitic stratovolcano.

Stratovolcano

Lava dome

10.1029/2004eo340001

Cite

Citations (26)

Magma chamber dynamics during the December 2008/January 2009 extrusion event at Soufriere Hills Volcano, Montserrat (W.I.), derived from strain data analysis

Geophysical Journal International (2011)

Stefanie Hautmann D. Hidayat Nicolas Fournier A. T. Linde I. Selwyn Sacks

Magma chamber

Strain (injury)

Source

Cite

Citations (0)

Pyroclastic Flow Generated Tsunami Waves Detected by CALIPSO Borehole Strainmeters at Soufriere Hills, Montserrat During Massive Dome Collapse: Numerical Simulations and Observations

AGUFM (2004)

E. J. van Boskirk B. Voight P. Watts Christina Widiwijayanti G. S. Mattioli

Dome (geology)

Source

Cite

Citations (1)

Eruptive Processes Leading to the Most explosive Lava fountain at Etna Volcano: The 23 November 2013 episode

EGUGA (2014)

Alessandro Bonaccorso Sonia Calvari A. T. Linde S. I. Sacks

The 23 November 2013 lava fountain at Etna volcano was the most explosive of the last 44 episodes that have occurred at Etna in 2011–2013. We infer the total magma volume erupted by thermal images analysis and show that it was characterized by a very high time-averaged-discharge-rate (TADR) of ~360 m3 s−1, having erupted ~1.6 × 106 m3 of dense-rock equivalent magma volume in just 45 min, which is more than 3 times the TADR observed during previous episodes. Two borehole dilatometers confirmed the eruption dynamics inferred from the thermal images. When compared to the other lava fountains, this episode can be considered as the explosive end-member. However, the erupted volume was still comparable to the other lava fountain events. We interpret that the 23 November explosive end-member event was caused by more primitive and gas-rich magma entering the system, as demonstrated by the exceptional height reached by the lava fountain.

Fountain

Effusive eruption

Lateral eruption

Source

Cite

Citations (0)

New data from borehole strainmeters to infer lava fountain sources (Etna 2011–2012)

Geophysical Research Letters (2013)

Alessandro Bonaccorso Gilda Currenti A. T. Linde S. I. Sacks

Abstract In January 2011, eruptive activity resumed at Etna producing a new phase with frequent lava fountain episodes until April 2012. In November 2011, the first two borehole strainmeters were installed, which detected negative strain changes (~0.15–0.8 μstrain) during the paroxysmal events. A Finite Element Model was set up to estimate accurately the tilt and volumetric strain, taking into account the real profile of the volcano and the elastic medium heterogeneity. The numerical computations indicated an elongated depressurizing source located at 0 km b.s.l., which underwent a volume change of ~2 × 10 6 m 3 which is the most of the magma volume erupted, while a smaller remaining part is accommodated by the magma compressibility. This shallow source cannot accumulate large magma volumes and, thus, favors short‐term periodic eruptive events with a fairly constant balance between the refilling and the erupted magma.

Magma chamber

10.1002/grl.50692

Cite

Citations (31)

Erratum: Slow earthquakes triggered by typhoons

Nature (2009)

ChiChing Liu A. T. Linde I. Selwyn Sacks

Typhoon

10.1038/nature08202

Cite

Citations (36)