2017
DOI: 10.1007/s10950-017-9700-2
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Earthquake precursors: spatial-temporal gravity changes before the great earthquakes in the Sichuan-Yunnan area

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Cited by 9 publications
(5 citation statements)
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“…No research conclusion can be referred to for the probability distribution form of the selected random sampling variables. However, if the expectation E(X) = µ and the variance D(X) = σ 2 > 0 of a random variable X, then for different values of the vector {X n }, when n is large enough (the sample size of 30 is generally considered to be sufficient), the mean value X n of {X n } will approximately obey a normal distribution, denoted as X n µ, σ 2 /n , as shown in Equation (3).…”
Section: Methods For Building the Sample Spacementioning
confidence: 99%
See 1 more Smart Citation
“…No research conclusion can be referred to for the probability distribution form of the selected random sampling variables. However, if the expectation E(X) = µ and the variance D(X) = σ 2 > 0 of a random variable X, then for different values of the vector {X n }, when n is large enough (the sample size of 30 is generally considered to be sufficient), the mean value X n of {X n } will approximately obey a normal distribution, denoted as X n µ, σ 2 /n , as shown in Equation (3).…”
Section: Methods For Building the Sample Spacementioning
confidence: 99%
“…The former is a data-driven method, and the reliability of the calculation results depends mainly on the accumulation of historical seismic hazard data. In contrast, there is still a need for more historical seismic hazard data [3,4], and their practical application is limited to a certain extent [5]. At the same time, the assessment results of this type of method are biased toward the macro, the assessment accuracy of individual needs to be improved, and it is difficult to reflect the differences between individual buildings of the same type.…”
Section: Introductionmentioning
confidence: 99%
“…In this study, the deep locking characteristics obtained by GPS data inversion from 1991 to 2018 in the middle and southern segments of the Tanlu fault zone showed that the Changyi-Tancheng and Wangji-Lujiang segments of the Tanlu fault zone are in a high degree of locking and a state of compression-slip deficit. According to historical records, the 7.0M Anqiu earthquake occurred in 70 BC in the Juxian section of Anqiu, but no seismic surface rupture zone related to the earthquake has been identified to date (Zhu et al, 1991;Wang et al, 2015). In addition, Cao et al (2018) used field geological surveys, shallow seismic exploration, combined borehole profiles, and palaeoseismic detection methods, and suggested that the deep structural detection of the Anqiu-Juxian member showed that the stress was released in the middle-and low-velocity layers of the crust.…”
Section: Sectional Seismic Risk Analysis Of the Mid-southern Segment ...mentioning
confidence: 99%
“…In recent years, the rapid development of high-precision absolute gravimeters has made available time-varying gravity data obtained by the terrestrial hybrid repeated gravity observation (THRGO) system, which have been applied to investigate crustal deformation, deep crustal fluid migration, and crustal apparent density variations in tectonically active regions [6,7]. Recently, relatively accurate medium-term predictions of several large earthquakes have been made by interpreting the data of anomalous gravity changes with reference to historical local earthquake records [8][9][10]. Many scholars therefore believe that it is possible to extract the gravity signals that are probably associated with deep mass transfer processes from THRGO records [11], which is the basis for applying time-varying gravity observations to in-depth explorations of earthquake mechanisms and seismic risk prediction [12].…”
Section: Introductionmentioning
confidence: 99%