@article{ref1,
title="The Aegean Sea (Greece) earthquake sequence of 25 March 1986: An application of the ν-value method for earthquake prediction",
journal="Natural hazards",
year="1989",
author="Papanastassiou, D. and Latoussakis, J. and Stavrakakis, G. and Drakopoulos, J.",
volume="2",
number="2",
pages="105-114",
abstract="A technique based on the ν-value, which is defined by % MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaWaaSGbaeaaca% GGOaGafqiXdqNbaebacaGGPaWaaWbaaSqabeaacaaIYaaaaaGcbaWa% a0aaaeaacqaHepaDdaahaaWcbeqaaiaaikdaaaaaaaaaaaa!3CEB![{{(bar tau )^2 } mathord{left/ {vphantom {{(bar tau )^2 } {overline {tau ^2 } }}} right. kern-nulldelimiterspace} {overline {tau ^2 } }}], where τ is the time interval between two adjacent earthquakes and indicates the pattern of time sequences of earthquakes, has been applied to the 25 March 1986 Aegean Sea (Greece) earthquake (M L = 5.2) in an attempt to discover temporal changes in seismicity. The analysis of several earthquake sequences revealed that low ν-values preceded the occurrence of relatively large earthquakes. The ν-value technique may be used for monitoring the seismicity changes.<p /><p>Language: en</p>",
language="en",
issn="0921-030X",
doi="10.1007/BF00141385",
url="http://dx.doi.org/10.1007/BF00141385"
}