Works matching IS 02787407 AND DT 2018 AND VI 37 AND IP 3
Results: 16
Spatial and Temporal Variations in the Moment Tensor Solutions of the 2008 Wenchuan Earthquake Aftershocks and Their Tectonic Implications.
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- Tectonics, 2018, v. 37, n. 3, p. 989, doi. 10.1002/2017TC004764
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Early Cenozoic Denudation of Central West Britain in Response to Transient and Permanent Uplift Above a Mantle Plume.
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- Tectonics, 2018, v. 37, n. 3, p. 914, doi. 10.1002/2017TC004796
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Three‐Dimensional Modeling of Mount Etna Volcano: Volume Assessment, Trend of Eruption Rates, and Geodynamic Significance.
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- Tectonics, 2018, v. 37, n. 3, p. 842, doi. 10.1002/2017TC004851
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Intrusion of Magmatic Bodies Into the Continental Crust: 3‐D Numerical Models.
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- Tectonics, 2018, v. 37, n. 3, p. 705, doi. 10.1002/2017TC004738
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Forearc Basin Stratigraphy and Interactions With Accretionary Wedge Growth According to the Critical Taper Concept.
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- Tectonics, 2018, v. 37, n. 3, p. 965, doi. 10.1002/2017TC004744
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Polyphased Inversions of an Intracontinental Rift: Case Study of the Marrakech High Atlas, Morocco.
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- Tectonics, 2018, v. 37, n. 3, p. 818, doi. 10.1002/2017TC004693
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Multiphase Structural Evolution of a Continental Margin During Obduction Orogeny: Insights From the Jebel Akhdar Dome, Oman Mountains.
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- Tectonics, 2018, v. 37, n. 3, p. 888, doi. 10.1002/2016TC004442
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Reconstructing Plate Boundaries in the Jurassic Neo‐Tethys From the East and West Vardar Ophiolites (Greece and Serbia).
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- Tectonics, 2018, v. 37, n. 3, p. 858, doi. 10.1002/2017TC004790
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Pre‐Alpine (Variscan) Inheritance: A Key for the Location of the Future Valaisan Basin (Western Alps).
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- Tectonics, 2018, v. 37, n. 3, p. 786, doi. 10.1002/2017TC004633
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Active Deformation of Malawi Rift's North Basin Hinge Zone Modulated by Reactivation of Preexisting Precambrian Shear Zone Fabric.
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- Tectonics, 2018, v. 37, n. 3, p. 683, doi. 10.1002/2017TC004628
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Reply to Comment by Vincent et al.
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- Tectonics, 2018, v. 37, n. 3, p. 1017, doi. 10.1002/2017TC004793
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Comment on “Relict Basin Closure and Crustal Shortening Budgets During Continental Collision: An Example From Caucasus Sediment Provenance” by Cowgill et al. (2016).
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- Tectonics, 2018, v. 37, n. 3, p. 1006, doi. 10.1002/2017TC004515
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Crustal‐Scale Fault Interaction at Rifted Margins and the Formation of Domain‐Bounding Breakaway Complexes: Insights From Offshore Norway.
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- Tectonics, 2018, v. 37, n. 3, p. 935, doi. 10.1002/2017TC004792
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Constraints Imposed by Rift Inheritance on the Compressional Reactivation of a Hyperextended Margin: Mapping Rift Domains in the North Iberian Margin and in the Cantabrian Mountains.
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- Tectonics, 2018, v. 37, n. 3, p. 758, doi. 10.1002/2016TC004454
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Thermochronometry Across the Austroalpine‐Pennine Boundary, Central Alps, Switzerland: Orogen‐Perpendicular Normal Fault Slip on a Major “Overthrust” and Its Implications for Orogenesis.
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- Tectonics, 2018, v. 37, n. 3, p. 724, doi. 10.1002/2017TC004619
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Issue Information.
- Published in:
- Tectonics, 2018, v. 37, n. 3, p. 681, doi. 10.1002/tect.20604
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- Article