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Table of Contents - Special Paper 269: |
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The South Tibetan Detachment System, Himalayan Orogen: Extension Contemporaneous with and Parallel to Shortening in a Collisional Mountain Belt |
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Foreword Abstract Introduction Geological Setting South Tibetan Detachment System Gyirong Area Nyalam Area Rocks of the Tibetan Sedimentary Sequence: Nyalam Structure of the Nyalam Area Structure of the Tibetan Sedimentary Sequence: Nyalam The Nyalam Detachment Kinematic Interpretation: Nyalam Qomolangma (Everest) Area Rocks of the Tibetan Sedimentary Sequence: Qomolangma Structure of the Qomolangma Area Structure of the Tibetan Sedimentary Sequence: Qomolangma The Qomolangma Detachment Kinematic Interpretation: Qomolangma Dinggyę Area Rocks of the Tibetan Sedimentary Sequence: Dinggyę Structure of the Dinggyę Area Structure of the Tibetan Sedimentary Sequence: Dinggyę Basal Detachments in the Dinggyę Area Late Structures Affecting All Units at Dinggyę Kinematic Interpretation: Dinggyę Wagye La Area Rocks of the Tibetan Sedimentary Sequence: Wagye La Cenozoic(?) Rocks in the Wagye La Area Structure of the Wagye La Area Structure of the Tibetan Sedimentary Sequence: Wagye La Structure of the Cenozoic(?) Sequence: Wagye La Contact Relations Between the Tibetan and Greater Himalayan Sequences at Wagye La Lhozhag-La Kang Area Structure of the Lhozhag-La Kang Area Structure of the Northern Segment: Lhozhag-La Kang Kinematic Interpretation: Lhozhag-La Kang Regional Geometry, Style, and Timing of Normal Faults Within Mapped Areas Magnitude of Displacement Related Extensional Structures Lateral Extent of the Detachment System Significance of the Himalayan Normal Faults Acknowledgments References Cited |