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PRESTo

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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1985
AAPG Bulletin (1985) 69 (9): 1434.
...George B. Carpenter Abstract: PRESTO (Probabilistic Resource ESTimates, OCS) is a computer program developed to provide resource estimates for offshore areas considered for leasing by the federal government. The program uses Monte Carlo simulation techniques to “drill” prospects...
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Figure  1 — 1,  Location of Bolivia in South America;  2,  location of the ...
Published: 01 November 2006
Figure 1 — 1, Location of Bolivia in South America; 2, location of the study area in Bolivia; 3, location of the Presto-El Peral, Candelaria, and Ayo Ayo sections; 4, detailed location of the Presto-El Peral section (arrow). The section is located 50 km northeast of Sucre, 35 km north
Journal Article
Published: 23 August 2017
Seismological Research Letters (2017) 88 (6): 1499–1507.
...M. Carranza; E. Buforn; A. Zollo ABSTRACT The process followed to configure the software PRESTo (PRobabilistic and Evolutionary early warning SysTem; University of Naples Federico II) to operate in the Ibero‐Maghrebian region (IMR) is described, and its performance in the first five months...
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Journal Article
Published: 03 January 2019
Seismological Research Letters (2019) 90 (2A): 530–538.
FIGURES | View All (5)
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Figure  9 — 1,  Zoophycos  isp., helicoidal form with an upward growth;  2,...
Published: 01 November 2006
Figure 9 — 1, Zoophycos isp., helicoidal form with an upward growth; 2, intense bioturbation by Zoophycos isp. Presto-El Peral section (Icla Formation); 3, Helminthopsis isp. and Zoophycos isp, Ayo Ayo section (Belen Formation, equivalent to the Icla Formation); 4, Phycosiphon
Journal Article
Journal: Clay Minerals
Published: 01 June 2012
Clay Minerals (2012) 47 (2): 243–250.
...-in-Aid for Precursory Research for Embryonic Science and Technology (PRESTO) from Japan Science and Technology Agency (JST). REFERENCES Chernia Z. Gill D. ( 1999 ) Flattening of TMPyP adsorbed on Laponite. Evidence in observed and caluculated UV-vis spectra . Langmuir , 15 , 1625...
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Overall performances of the network‐based (<b>PRESTo</b> v.1.0) and the stand‐alon...
Published: 22 November 2017
Figure 5. Overall performances of the network‐based (PRESTo v.1.0) and the stand‐alone (SAVE v.1.0) EEWS. (a) Histogram of the number of available stations as a function of the distance; (b) rate of SA, SNA, MA, and FA using PRESTo v.1.0 as a function of the distance. (c) Rate of SA, SNA, MA
Journal Article
Journal: Clay Minerals
Published: 01 June 1999
Clay Minerals (1999) 34 (2): 213–220.
Journal Article
Journal: Clay Minerals
Published: 01 December 1998
Clay Minerals (1998) 33 (4): 643–650.
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Timeline of the playback of the 2013  M  4.9 Matese earthquake. (a) An evol...
Published: 18 February 2015
Figure 9. Timeline of the playback of the 2013 M  4.9 Matese earthquake. (a) An evolutionary event characterization by regional PRESTo Plus EEWS and messages received by the Sentinel at MAJI. Marker locations over the timeline are approximate only. (b)  EEW messages transmitted by PRESTo Plus
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Performances of the network‐based (<b>PRESTo</b> v.1.0) and stand‐alone (on‐Site‐A...
Published: 22 November 2017
Figure 4. Performances of the network‐based (PRESTo v.1.0) and stand‐alone (on‐Site‐Alert‐leVEl [SAVE] v.1.0) earthquake early warning system (EEWS) for the M w  6.5 Norcia earthquake. (a) Areal distribution of successful alerts (SA), successful no‐alerts (SNA), missed alerts (MA
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(a) Screenshot of the playback in <b>PRESTo</b> Plus  of the waveforms recorded by...
Published: 18 February 2015
Figure 8. (a) Screenshot of the playback in PRESTo Plus of the waveforms recorded by ISNet and the MAJ3 station (i.e., MAJI in the subplot) during the M  4.9 Matese earthquake. The MAJ3 recording is on the forefront in the left part, with S ‐waves (dark gray) evidenced. The screenshot shows
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Figure  2 —The stratigraphic section at <b>Presto</b>-El Peral
Published: 01 November 2006
Figure 2 —The stratigraphic section at Presto-El Peral
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<b>PRESTo</b> Plus  flow chart (modified from  Zollo  et al. , 2010 ).
Published: 18 February 2015
Figure 3. PRESTo Plus flow chart (modified from Zollo et al. , 2010 ).
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(a) Epicentral location of earthquakes detected by <b>PRESTo</b> (PRobabilistic an...
Published: 23 August 2017
Figure 1. (a) Epicentral location of earthquakes detected by PRESTo (PRobabilistic and Evolutionary early warning SysTem) in real time (white circles), false detections (white squares), undetected earthquakes (gray circles), and the receiving seismic stations (black triangles). The white star
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Number of earthquakes versus differences between <b>PRESTo</b> and Instituto Geogr...
Published: 23 August 2017
Figure 3. Number of earthquakes versus differences between PRESTo and Instituto Geográfico Nacional (IGN) estimates for (a) epicenter, (b) depth, (c) origin time, and (d) magnitude, distinguishing the first alert estimate (gray bars) and the final estimate (white bars).
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Epicentral location of <b>PRESTo</b> first alert (black star) and end time (white ...
Published: 23 August 2017
Figure 4. Epicentral location of PRESTo first alert (black star) and end time (white star), and IGN (black circle) for the (a) 25 January 2016 and (b) 23 January 2016 earthquakes. Black squares represent the 10 cities closest to the epicenter. Black triangles correspond to the stations that were
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1–3,  Bolithes crasquinae n. gen., n. sp., <b>Presto</b>-El Peral section, Icla Fo...
Published: 01 November 2011
F igure 3 1–3, Bolithes crasquinae n. gen., n. sp., Presto-El Peral section, Icla Formation. 1, dorsum with operculum opened, FCGI 3585, ×7.8; 2, external mold of conch with operculum apparently opened, with cross-section of external molds of conchs next to it, FCGI 3586, ×16; 3, three
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Figure  10 —Preferential orientation of  Diplocraterion parallelum  at the ...
Published: 01 November 2006
Figure 10 —Preferential orientation of Diplocraterion parallelum at the top of a rippled bed, Presto-El Peral section (Santa Rosa Formation)
Journal Article
Published: 24 March 2021
Seismological Research Letters (2021) 92 (4): 2321–2332.
...‐time residuals, etc.). Velocity models input to the PRESTo algorithm are region specific. The velocity models used for ITA and PYR are the same as those adopted for the generation of synthetic seismograms in both testbeds (see the Considered events section). We use the Tryggvason et al. (2002...
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