(Q57075335)

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The Eocene Southern Vancouver Island Orocline — a response to seamount accretion and the cause of fold-and-thrust belt and extensional basin formation

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The Eocene Southern Vancouver Island Orocline — a response to seamount accretion and the cause of fold-and-thrust belt and extensional basin formation (English)

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Stephen T. Johnston

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Shannon Acton

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publication date

April 2003

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365

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1-4

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165-183

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A rifted margin origin for the crescent basalts and related rocks in the northern Coast Range Volcanic Province, Washington and British Columbia

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Paleomagnetism of small basalt exposures in the West Puget Sound Area, Washington, and Speculations on the accretionary origin of the Olympic Mountains

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Seismic reflection constraints on imbrication and underplating of the northern Cascadia convergent margin

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LITHOPROBE—southern Vancouver Island: Cenozoic subduction complex imaged by deep seismic reflections

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A captured island chain in the coast range of Oregon and Washington

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Fission-track dating of the tectonic development of the San Juan Islands, Washington

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The Great Alaskan Terrane Wreck: reconciliation of paleomagnetic and geological data in the northern Cordillera

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Yellowstone in Yukon: The Late Cretaceous Carmacks Group

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Metchosin Igneous Complex, southern Vancouver Island: Ophiolite stratigraphy developed in an emergent island setting

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Evolution of the Pacific Margin, Vancouver Island, and adjacent regions

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Oroclinal bending and evidence against the Pangea megashear: The Cantabria-Asturias arc (northern Spain)

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10.1016/S0040-1951(03)00021-0

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2003Tectp.365..165J

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