The Neftegorsk 1995 May 27 earthquake (M-S = 7.6) occurred in the northern
part of Sakhalin Island in a region considered to be a fairly inactive plat
e boundary between the North American and Eurasian plates. Coseismic surfac
e ruptures are associated with the Upper Piltoun fault, a secondary feature
joining the Sakhalin-Hokkaido and Middle Sakhalin faults, which are the ma
in tectonic elements of the region. Observations obtained during a field ex
periment that included a local seismic network, neotectonics and geodetic m
easurements are combined with the analysis of satellite images and a broad-
band body wave inversion. A complex source model consisting of four branche
s is proposed. The two main branches, oriented N-S, show right-lateral stri
ke-slip motion. The rupture nucleates between these two segments and propag
ates bilaterally. We estimate a total rupture length of 46 km, a width of 1
2 km, and an average slip value of 3.9 m. However, the maximum observed val
ue of surface slip is 8.1 m, an unusually large value for an event of this
magnitude. This earthquake supports the model of a North American plate rot
ating clockwise with respect to Eurasia.