.... The lack of small events in the Rotenburg region is striking and adequately supports the nontectonic origin. For the earthquakes induced in the Rotliegend rocks of the Netherlands, the Bergermer field has experienced four larger earthquakes with magnitudes 3.2 ≤ M ≤ 3.5 and no events smaller than M 3...

... in the Groningen gas field and for seismicity induced in the Bergermeer underground gas storage system. It has, however, also been noted that the efficiency of TLS control of gas production–induced seismicity is not generally accepted ( Muntendam‐Bos et al. , 2015 ). Despite their widespread application...

.... Three fields so far have had induced events with magnitudes above 3.0 — Bergermeer (as high as 3.5), Groningen (as high as 3.6), and Roswinkel (as high as 3.4) ( Figure 1a ). Figure 1. (a) Overview of Dutch oil and gas fields and the seismicity induced by gas extraction. (b) Overview of the Dutch...

..., induced seismicity in connection to geologic carbon sequestration projects has emerged as a new field of interest. This review discusses seismicity induced by hydrocarbon production. In particular, I focus on published cases for which earthquakes of moderate-to-large magnitudes-in other words earthquakes...

... by companies other than NAM in 1972. Amoco drilled 4 development wells in the Bergermeer gas field, for a total of 13,700 m. Three wells were gas producers and the fourth was completed as a water-injection well. Gas production commenced in October from the Bergermeer field, but 2 other small fields on Amoco’s...

... production-related earthquake detected within the Groningen field was in 1991. To date, there have been 17 Richter local magnitude (M L ) ≥ 3.0 earthquakes in the northern Netherlands: nine in the Groningen field, four in the Bergermeer field, and three in the Roswinkel field ( Royal Netherlands...

..., and Middelie oil fields; Bergermeer, Groet, Akkrum, Coevorden, Wanneperveen, Tietjdeel, Tubbergen, Blijham, Dalen, Emmen, Emmen-Nieuwe Amsterdam, Roswinkel, Sleen, Harkstede, Kooipolder, t’Zandt, Zuidbroek, Leeuwarden, Nijega, Ried, and Opeinde gas fields). Ultimate total recovery from the Schoonebeek oil...

... resulted from the Dutch government’s policy of Groningen gas conservation. The bulk of the increased production is believed to have come from Ameland, Bergen, Bergermeer, Coevorden, De Wijk-Wanneperveen, Rossum-De Lutte, and Zuidwal fields. Oil reserves increased about 5% as a result of the Pernis...

... concession beyond the limits of the Groningen gas field. Rustenburg 1 (drilled in 1976) was southeast of Amoco’s Bergermeer field in Noord Holland, and Landsmeer 1 was south of there in the northeast outskirts of Amsterdam. Presumably all 4 of these discoveries were from the Permian. An interesting well...

... to the Bergen field, Bergermeer No. 1. Six attempts to extend gas production of the Leeuwarden area and 1 of Akkrum were unsuccessful, emphasizing the local structural and stratigraphic complexity of central Friesland. Amoco, Petroland, and Texaco-Chevron carried out 11 party-months of seismic work...

... in the Rotliegend in Noord Holland and 1 in the Lower Cretaceous near the Leeuwarden gas field in Friesland. Amoco abandoned Starnmeer 1, which was drilled in 1974, and drilled 2 additional wells south of the Bergermeer gas field, of which Aklmaar 1, was a gas discovery. Petroland carried out 5 months of seismic...

... or three times lower than laboratory analyses on the same samples, were found to be related to absolute concentrations closely enough to rank samples. In order to investigate further the feasibility of field analyses on wet sediments, partial dehydration methods were tested. The most efficient technique...

... by seismogenic sea waves happening in a closed gulf, far away from the open ocean. Eyewitness reports, field observations, and a mareogram recorded near Elat demonstrated conclusively that tsunami hazard in the GOE deserves focused attention. Here we take up the challenge, adopting the GeoClaw package...

...Diego Melgar; Angel Ruiz‐Angulo; Brendan W. Crowell; Eric J. Fielding; Ericka A. Solano‐Hernandez ABSTRACT We present a slip model for the 2021 M 7 Acapulco, Mexico, earthquake produced by inversion of strong motion, Global Navigation Satellite Systems, tide gauge, and Interferometric Synthetic...

.... The objective is to test an algorithm we have developed that relies on a method described in Singh et al. (2012) based on real‐time to near real‐time estimates of the static‐displacement field (ideally measured from a Global Positioning System [ GPS ]). We analyze synthetic‐displacement time series...

...Breanyn T. MacInnes; Aditya Riadi Gusman; Randall J. LeVeque; Yuichiro Tanioka Abstract Selection of the earthquake source used in tsunami models of the 2011 Tohoku event affects the simulated tsunami waveform across the near field. Different earthquake sources, based on inversions of seismic...

... to analyse small areas and detection limits in the ppm range have made it particularly alluring to these fields of study. Another successful application is in the analysis of alloys, the technique having specific methods for this material. A search, using the search engine SCOPUS, of >7200 journals...

... ( Blewett et al. , 2012 ), subduction of oceanic crust along the southern coast of Java began ( Hall, 2011 ) and has continued to the present day, creating a north–south‐directed maximum stress and generating the late Neogene Sunda orogeny ( Simandjuntak and Barber, 1996 ). This stress field generated east...

... detail on field context, petrography and other relevant information. Importantly, when the REE + Y are normalized with local tonalite ( Berger & Rollinson 1997 ), the slope is rotated and the pattern becomes familiar ( Fig. 3 ). Because the tonalites themselves have a pronounced Eu depletion...