A hybrid method for calculating the radiated wave energy of deep earthquakes
n.w.winslow l.j.ruff

..............page:52-60

Seimic hazard in the Marmara Sea region following the 17 August 1999 Izmit earthquake
a. hubert-ferrari a. barka e. jacques s.s. nalbant b. meyer r. armijo p. tapponnier g.c.p. king

..............page:17-23

Probability of a great earthquake to recur in the Tokai district, Japan: reevaluation based on newly-developed paleoseismology, plate tectonics, tsunami study, micro-seismicity and geodetic measurements
t. rikitake

..............page:6-16,23

Экспериментальные исследования электромагнитного поля СНЧ-радиоустановки для целей мониторинга сейсмической активности на Северно
. . . . . . . . . .

..............page:61-67

Strength of the San Andreas
m. d. zoback

..............page:87-89

Coseismic spring flow changes associated with the 1995 Kobe earthquake
t. sato r. sakai k. furuya t. kodama

..............page:81-84

Further evidence for the compound nature of slow earthquakes:The Prince Edward Island earthquake of April 28,1997
j.j.mcguire t.h.jordan

..............page:44-51

Conditions for earthquake surface rupture along the San Andreas fault system, California
j. e. styeit

..............page:32-43

Underdamped responses of a well to nearby swarm earthquakes off the coast of Ito City, central Japan, 1995
t. kunugi y. fukao m. ohno

..............page:68-80

Estimation of seismic hazard parameters for the Himalayas and its vicinity from complete data files
d. shanker m.l. sharma

..............page:24-31

di zhen zai hai fang yu gong zuo de jin zhan
lv chun lai ; chen ying fang

..............page:1-5

Inner core takes another turn
h-c. nataf

..............page:85-86