Foreword
Abstract
Introduction
Background
Sections of the rupture
Summary of surface faulting in 1957
Implications for characteristic earthquakes, triggering of ruptures, and
earthquakes elsewhere
Implications for recurrence intervals of major earthquakes and rates of
deformation in the Gobi-Altay
Implications for intracontinental mountain building
Acknowledgments
Appendix A: Sites where detailed topographic maps and profiles were made to quantify offsets
along the surface rupture of the 1957 Gobi-Altay earthquake in Mongolia
References cited |