Geodynamics of trench advance: Insights from a Philippine-Sea-style geometry
暂无分享,去创建一个
[1] S. Kramer,et al. Interaction of subducted slabs with the mantle transition‐zone: A regime diagram from 2‐D thermo‐mechanical models with a mobile trench and an overriding plate , 2014 .
[2] R. Arculus,et al. 40Ar/ 39Ar and K–Ar geochronological age constraints for the inception and early evolution of the Izu–Bonin – Mariana arc system , 1998 .
[3] N. Ribe. Bending mechanics and mode selection in free subduction: a thin-sheet analysis , 2010 .
[4] A. Beck. Heat Flow , 2015 .
[5] Shin-Chan Han,et al. Source parameter inversion for recent great earthquakes from a decade‐long observation of global gravity fields , 2013 .
[6] C. Kreemer,et al. Absolute plate velocities from seismic anisotropy: Importance of correlated errors , 2014 .
[7] E. Okal,et al. A global survey of stress orientations in subducting slabs as revealed by intermediate‐depth earthquakes , 2004 .
[8] T. Gerya,et al. Geodynamic regimes of intra-oceanic subduction: Implications for arc extension vs. shortening processes , 2014 .
[9] H. Čížková,et al. The viscosity of Earth's lower mantle inferred from sinking speed of subducted lithosphere , 2012 .
[10] R. Carlson,et al. Characteristics of back-arc regions , 1984 .
[11] Richard G. Gordon,et al. Geologically current plate motions , 2010 .
[12] H. Čížková,et al. Effects of mantle and subduction-interface rheologies on slab stagnation and trench rollback , 2013 .
[13] H. Čížková,et al. Long-wavelength character of subducted slabs in the lower mantle , 2008 .
[14] D. Stegman,et al. A regime diagram for subduction styles from 3-D numerical models of free subduction , 2010 .
[15] R. Boehler,et al. Thermal expansivity in the lower mantle , 1992 .
[16] B. Taylor,et al. Rifting and the Volcanic-Tectonic Evolution of the Izu-Bonin-Mariana Arc , 1992 .
[17] L. Handayani. Seismic tomography constraints on reconstructing the Philippine Sea Plate and its margin , 2005 .
[18] Y. Fukao,et al. Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity , 2012 .
[19] G. Hirth,et al. Rheology of the Upper Mantle and the Mantle Wedge: A View from the Experimentalists , 2013 .
[20] George Helffrich,et al. Phase transition Clapeyron slopes and transition zone seismic discontinuity topography , 1994 .
[21] R. Carlson,et al. Subduction hinge migration , 1984 .
[22] Walter R. Roest,et al. Age, spreading rates, and spreading asymmetry of the world's ocean crust , 2008 .
[23] G. Morra,et al. The role of elasticity in slab bending , 2014 .
[24] S. Uyeda,et al. Heat flow in the Philippine Sea , 1970 .
[25] Simon L. Klemperer,et al. An Overview of the Izu‐Bonin‐Mariana Subduction Factory , 2013 .
[26] C. Thieulot,et al. Influence of surrounding plates on 3D subduction dynamics , 2009 .
[27] R. Larter,et al. Intra-Oceanic Subduction Systems: Tectonic and Magmatic Processes , 2003 .
[28] E. Bataillon. Geodynamic setting of Izu-Bonin-Mariana boninites , 2007 .
[29] M. Sudo,et al. Initiation and propagation of subduction along the Philippine Trench: evidence from the temporal and spatial distribution of volcanoes , 2004 .
[30] Arie P. van den Berg,et al. On the role of subducting oceanic plateaus in the development of shallow flat subduction , 2002 .
[31] D. Yuen,et al. The effects of temperature-dependent viscosity on mantle convection with the two major phase transitions , 1995 .
[32] Y. Iryu,et al. Philippine Sea Plate motion since the Eocene estimated from paleomagnetism of seafloor drill cores and gravity cores , 2010 .
[33] N. Bellahsen,et al. Dynamics of Subduction and Plate Motion in Laboratory Experiments. , 2004 .
[34] J. Hunen,et al. Collisional processes and links to episodic changes in subduction zones. , 2015 .
[35] J. Ali,et al. Philippine Sea Plate motion history: Eocene-Recent record from ODP Site 1201, central West Philippine Basin , 2015 .
[36] L. Royden,et al. Anomalously fast convergence of India and Eurasia caused by double subduction , 2015 .
[37] Hua-Wei Zhou. Mapping of P-wave slab anomalies beneath the Tonga, Kermadec and New Hebrides arcs , 1990 .
[38] D. Stegman,et al. Global trench migration velocities and slab migration induced upper mantle volume fluxes: Constraints to find an Earth reference frame based on minimizing viscous dissipation , 2008 .
[39] David A. Yuen,et al. The effects of a composite non-Newtonian and Newtonian rheology on mantle convection , 1993 .
[40] T. Geenen,et al. Using open sidewalls for modelling self-consistent lithosphere subduction dynamics , 2012 .
[41] C. Faccenna,et al. Trench migration, net rotation and slab-mantle coupling , 2008 .
[42] Dapeng Zhao,et al. High‐resolution mantle tomography of China and surrounding regions , 2006 .
[43] H. Čížková,et al. Stress distribution within subducting slabs and their deformation in the transition zone , 2007 .
[44] K. Otsuki. Westward migration of the Izu-Bonin Trench, northward motion of the Philippine Sea Plate, and their relationships to the Cenozoic tectonics of Japanese island arcs , 1990 .
[45] Gavin P. Hayes,et al. Seismicity of the Earth 1900-2012 Philippine Sea plate and vicinity , 2013 .
[46] H. Čížková,et al. The effects of rheological decoupling on slab deformation in the Earth’s upper mantle , 2013, Studia Geophysica et Geodaetica.
[47] T. Yoshino,et al. P‐V‐T relations of MgSiO3 perovskite determined by in situ X‐ray diffraction using a large‐volume high‐pressure apparatus , 2009 .
[48] M. Billen. Slab dynamics in the transition zone , 2010 .