Titlebook: How to Study Global Christianity; A Short Guide for St Jason Bruner Textbook 2022 The Editor(s) (if applicable) and The Author(s), under ex

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Decolonizationhas been addressed within the anthropology of Christianity. This section will make some suggestions toward bridging that gap by asking what it means to think of Christianity worldwide in light of the questioning of the category of “religion” (e.g., Talal Asad, Saba Mahmood, and David Chidester). It

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heir use have been in the past and might be in the future. In addition to identifying themes within the discourse, this book offers a survey of where the field has been, what its analytical priorities are, and how future scholars might develop new research projects and trajectories in light of the its history.978-3-031-12810-3978-3-031-12811-0

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Jason Brunergeometry of polycrystalline quartz aggregates, extensional crenulation cleavages (ECCs), and quartz c-axis fabrics do not indicate any consistent preferred sense of movement. Both macro-and microstructural analyses suggest an inhomogeneous pure shear or flattening as the main deformation process rel

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olves a basement complex and Middle to Late Proterozoic strata. It is composed of two oblique-slip to frontal embryonic fold-thrust belts, which root in a central strike-slip system. The Espinha?o fold-thrust belt and the Paramirim corridor represent inverted segments of a Middle to Late Proterozoic

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Jason Brunerolves a basement complex and Middle to Late Proterozoic strata. It is composed of two oblique-slip to frontal embryonic fold-thrust belts, which root in a central strike-slip system. The Espinha?o fold-thrust belt and the Paramirim corridor represent inverted segments of a Middle to Late Proterozoic

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Jason Brunerower crustal zone and underlies most of the Newfoundland offshore structural elements. A linked system of synthetic and antithetic faults associated with this crustal detachment now borders the structural units of the shelf..The widespread reactivation of pre-existing Precambrian and Paleozoic zones

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uthern Appalachian highlands, the Arkansas-St. Lawrence lowland and the Mid-Continent Arch. The north-trending extensional faults appear related to right-lateral strike slip along the north west-trending zones. They are most prominent in the Great Basin in the west, but are also present in the east,