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Volume 10, Number 6
1 December 2018
Lithosphere Cover Image for Volume 10, Issue 6
ISSN: 1941-8264
EISSN: 1947-4253
In this Issue

RESEARCH

Early Paleozoic slab rollback in the North Altun, Northwest China: New evidence from mafic intrusions and high-Mg andesites
Xian-Tao Ye; Chuan-Lin Zhang; Ai-Guo Wang; Bin Wu; Guo-Dong Wang
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Time scale for the development of thickened crust in the Cretaceous North Cascades magmatic arc, Washington, and relationship to Cretaceous flare-up magmatism
Erin K. Shea; Jonathan S. Miller; Robert B. Miller; Christine F. Chan; Adam J.R. Kent; John M. Hanchar; Kelly Dustin; Scott Elkins
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Orocopia Schist in the northern Plomosa Mountains, west-central Arizona: A Laramide subduction complex exhumed in a Miocene metamorphic core complex
E.D. Strickland; J.S. Singleton; G.B. Haxel
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Geodynamics of Cenozoic extension along a transect across the Colorado River extensional corridor, southwestern USA
Jon E. Spencer; John S. Singleton; Evan Strickland; Stephen J. Reynolds; Diane Love; David A. Foster; Roy Johnson
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Structural evolution of a crustal-scale shear zone through a decreasing temperature regime: The Yukon River shear zone, Yukon-Tanana terrane, Northern Cordillera
A.J. Parsons; M.J. Coleman; J.J. Ryan; A. Zagorevski; N.L. Joyce; H.D. Gibson; K.P. Larson
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Earliest sedimentological evidence for marine ingressions in the eastern North American rift system, Central Atlantic Margin
Darragh O’Connor; Ricardo L. Silva; Grant Wach
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Eocene Basalt of Summit Creek: Slab breakoff magmatism in the central Washington Cascades, USA
Lisa B. Kant; Jeffrey H. Tepper; Michael P. Eddy; Bruce K. Nelson
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Dating growth strata and basin fill by combining 26Al/10Be burial dating and magnetostratigraphy: Constraining active deformation in the Pamir–Tian Shan convergence zone, NW China
Jessica Ann Thompson Jobe; Tao Li; Bodo Bookhagen; Jie Chen; Douglas Burbank
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  • Cover Image

    Cover Image

    issue cover

    COVER: Interleaved carbonate and quartzo-feldspathic metamorphic rocks in the immediate footwall of the Plomosa detachment fault. Note that the carbonate is plastically deformed whereas the quartzo-feldspathic rocks are much more strongly affected by brittle deformation. This would be expected for slow rock deformation at 200–300 °C. See “Geodynamics of Cenozoic extension along a transect across the Colorado River extensional corridor, southwestern USA” by Jon E. Spencer, John S. Singleton, Evan Strickland, Stephen J. Reynolds, Diane Love, David A. Foster, and Roy Johnson, https://doi.org/10.1130/L1002.1.

    PHOTO BY: Jon E. Spencer

    COVER DESIGN BY: Heather L. Sutphin

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