Neotectonics and tectonic stresses of the Sakhalin Island

Abstract

Abstract:The paper describes the neotectonics of the Sakhalin Island and analyzes the latest and recent tectonic stresses in the study area in order to establish their differences in the Amur and Okhotsk microplates, which boundary is confined to the Tym-Poronaisk fault, the largest NS-striking fault in the Central Sakhalin (Fig. 1). Our map of the structural geomorphological features of the study area (Fig. 2) shows three longitudinal zones: the western and eastern uplifts, and the Central Sakhalin basin between the uplifts. In the Southern Sakhalin, neotectonic stresses were studied by a combination of tectonophysical methods and the method of structural geology (Figures 3 to 6, and Table). Our study shows that the regional axes of maximum and minimum compressive principal normal stresses are primarily of the subhorizontal orientations (Fig. 5, Д). In the Northern and Central Sakhalin, neotectonic stresses were reconstructed by the structural geomorphology method. The compression axes are oriented sublatitudinally, with the NE-trending strike in the Northern Sakhalin (Fig. 7, A), and the extension axes are oriented submeridionally; in the Northern Sakhalin, respectively, they are oriented in the NW direction. The results of our study of neotectonic stresses were used to construct a map of recent geodynamics of Sakhalin (Fig. 7, Б), which shows zones differing in the geodynamic settings of the most recent faulting. According to the analysis of the recent tectonic stress with respect to the earthquake focal mechanisms in the period from 1978 to 2015 (Fig. 8), recent stresses dominating in Sakhalin have mainly the sublatitudinal low-angle orientations of the deviatoric compression axis. The submeridional low-angle orientations of the deviatoric extension axes are observed in the Northern Sakhalin and partly in the north of the Southern Sakhalin (see Fig. 8). The high-angle axes of deviatoric extension are typical of the western and central parts of the Southern Sakhalin, and such extension leads to horizontal compression and reverse faulting. In some areas of the recent stress field, the deviatoric axes of compression and extension have unstable orientations. The latitudinal boundaries of such areas are nearly coincident with the boundaries of the zones that differ in the geodynamic settings of the most recent faulting, which means that these areas and zones are reliably identified. The relative inhomogeneity of the neotectonic and recent stress fields in the Southern Sakhalin does not give grounds to distinguish differences in the state of crustal stresses in the areas located on the sides of the Southern Sakhalin fault. As a consequence, a boundary between the Amur and the Okhotsk Plate in the South Sakhalin cannot be drawn along this fault. It is most likely that this boundary coincides with the Western-Sakhalin fault in the southern areas of the study region. Our data on the Central and Northern Sakhalin does not contradict with the conclusion in [Savostin et al., 1982] concerning this boundary.

Earth Surface Deformation of the Sakhalin Island From GPS Data

“…Стрелками показаны скорости схождения литосферных плит в пределах о. Сахалин относительно Евразии. (б) -схема районирования областей с разной геодинамической обстановкой [Sim et al, 2017a].…”

“…The arrows show the rates of convergence of the lithospheric plates within the Sakhalin Island in relation to Eurasia. (б) -zoning of the areas with different geodynamic settings [Sim et al, 2017a].…”

“…Основным источником сведений о напряженнодеформированном состоянии являются данные о механизмах очагов землетрясений. Его детальному исследованию посвящены работы [Konovalov et al, 2014;Sim et al, 2017aSim et al, , 2017bTataurova, 2015], в которых выполнена реконструкция напряжений и деформаций на основе современной сейсмичности о. Сахалин. Показано, что территория острова в целом характеризуется субширотным сжатием, что соответствует современному тектоническому режиму региона.…”

“…Оси сжатия ориентированы субширотно, растяжения -субмеридионально. Такой комплексный анализ позволил откартировать районы с различной геодинамической обстановкой [Sim et al, 2017a[Sim et al, , 2017b.…”

Rifts, orogens, cratons, and global tectonics: Introduction

“…По структурным наблюдениям в Западно-Сахалинском террейне обозначена важ-нейшая роль правосторонних сдвиговых смещений по субмеридиональным разломам, которые, как предполагалось, имели место с эоцена до начала четвертичного периода [Golozubov et al, 2012[Golozubov et al, , 2016. Новые результаты структурных исследований на о-ве Сахалин, изложенные в статье [Sim et al, 2017], привели авторов к выводу о преобладании сдвиго-вого поля неотектонических напряжений с мери-диональной ориентировкой оси растяжения и ши-ротной -оси сжатия со сменой ориентировки на Северном Сахалине на северо-восточную. В финале зафиксировано взбросовое поле напряжений.…”