Δευτέρα, 4 Οκτωβρίου 2010
Νέα προσθήκη της ομάδας ΒΑΝ
Νεα συμπληρωματικά στοιχεία ανάρτησε η ομάδα ΒΑΝ στην σελίδα του πανεπιστημίου του Κορνέλ. Το πλήρες κείμενο (στα αγγλικά) είναι το πιο κάτω.
Note added on October 1, 2010: This is just a continu-
ation of the analysis started, as mentioned in the previ-
ous Note, in the area N(37.6-39.0) E(20.4-23.2) which is
now extended to N(37.5-38.8) E(19.8-23.3). At 03:53 UT
on September 2, 2010 a Ms(ATH)=4.8 earthquake actu-
ally occurred with an epicenter at 38.22N 23.17E, i.e., in-
side the area studied. In addition, upon the occurrence of
a ML =3.1 event at 15:42 UT on September 29, 2010 with
an epicenter at 37.56N 20.00E, when plotting the proba-
bility Prob( 1) versus 1, for Mthres=3.1, we find a sharp
maximum at 1 0.070 depicted in Fig.6, which probably
indicates that the critical point has been approached. To
ensure that this is a true criticality condition, the extent
to which a magnitude threshold invariance holds for this
result is currently investigated.
ation of the analysis started, as mentioned in the previ-
ous Note, in the area N(37.6-39.0) E(20.4-23.2) which is
now extended to N(37.5-38.8) E(19.8-23.3). At 03:53 UT
on September 2, 2010 a Ms(ATH)=4.8 earthquake actu-
ally occurred with an epicenter at 38.22N 23.17E, i.e., in-
side the area studied. In addition, upon the occurrence of
a ML =3.1 event at 15:42 UT on September 29, 2010 with
an epicenter at 37.56N 20.00E, when plotting the proba-
bility Prob( 1) versus 1, for Mthres=3.1, we find a sharp
maximum at 1 0.070 depicted in Fig.6, which probably
indicates that the critical point has been approached. To
ensure that this is a true criticality condition, the extent
to which a magnitude threshold invariance holds for this
result is currently investigated.
Δεν υπάρχουν σχόλια:
Δημοσίευση σχολίου