Table of Contents - SPE281: Geological and Geophysical Evidence for Deep Subduction of Continental Crust Beneath the Pamir
Acknowledgments
Abstract
Introduction
Geological Constraints on the Magnitude of Convergence Between the Pamir and the Rest of Eurasia
Bounds on the Present and Initial Crustal Thicknesses
Isostasy, Seismic Refraction, and Present Crustal Thicknesses
Subsidence of the Tadjik Depression Inferred from Stratigraphic Sections
Active and Quaternary Deformation
Shallow-Focus Seismicity and Fault Plane Solutions of Earthquakes
Geologic, Geomorphic, and Archaeologic Evidence for Recent Deformation
Active Faults Along the Western Margin of the Pamir
The Trans-Alai Belt of Active Faulting
Active Faulting Along the North Slope of the Western
Peter the First Range
Active Faults in the Tadjik Depression
Active Faults Within the High Pamir
Summary of Quaternary and Holocene Faulting
Geodetic Evidence of Rates of Deformation in the Garm Region
Runou Valley
Sari-Pul' Network
Regional Triangulation and Trilateration Network
Summary of Geodetic Results
Partitioning of India's Convergence with Eurasia Across the Pamir
Intermediate-Depth Seismicity, Upper Mantle Structure, and Evidence of Subducted Lithosphere
Summary and Synthesis
Appendix A: Discussion of Earthquakes in the Pamir Region
References Cited