what is a diffuse boundary plate tectonics

On the Evolution of Motion Across Diffuse Plate Boundaries. The impact of HRM digitalization on firm performance: investigating three‐way interactions.

The quest for wisdom: lessons from 17 tsunamis, 2004–2014.

Evolution of the eastern Indian Ocean since the Late Cretaceous: Constraints from Geosat altimetry. Sedimentation and tectonics of a diffuse plate boundary: the Canadian Arctic Islands from 80 Ma B.P. title = "A diffuse plate boundary model for Indian Ocean tectonics". Marine tectonics: Processes at mid‐ocean ridges. Multi‐fault rupture and successive triggering during the 2012 Mw 8.6 Sumatra offshore earthquake. This boundary, which trends E‐W from the Central Indian Ridge near Chagos Bank to the Ninetyeast Ridge, and north along the Ninetyeast Ridge to the Sumatra Trench, is a zone of concentrated seismicity and deformation heretofore characterized as “intraplate”. The rotation vector of Australia relative to Indo‐Arabia is consistent with the seismologically observed ∼2 cm/yr of left‐lateral strike‐slip along the Ninetyeast Ridge, N‐S compression in the Central Indian Ocean, and the N‐S extension near Chagos. This boundary, possibly initiated in late Miocene time, may be related to the opening of the Gulf of Aden and the uplift of the Himalayas. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. Depth‐Scanning Algorithm: Accurate, Automatic, and Efficient Determination of Focal Depths for Local and Regional Earthquakes. Constraints on hydrothermal heat flux through the oceanic lithosphere from global heat flow. caused by Labrador Sea-Baffin Bay spreading.

The rotation vector of Australia relative to Indo‐Arabia is consistent with the seismologically observed ∼2 cm/yr of left‐lateral strike‐slip along the Ninetyeast Ridge, N‐S compression in the Central Indian Ocean, and the N‐S extension near Chagos. Sections of the crust, called plates, push against each other due to forces from the molten interior of the Earth.

Geoid height versus topography of the Northern Ninetyeast Ridge: implications on crustal compensation. "Centroid depths and mechanisms of mid‐ocean ridge earthquakes in the Indian Ocean. The 2012 Mw 8.6 Sumatra earthquake: Evidence of westward sequential seismic ruptures associated to the reactivation of a N‐S ocean fabric. Planets, Magnetospheric Australia and India are conventionally thought to be contained in a single plate divided from an Arabian plate by the Owen Fracture Zone. The misclosure of the Indian Ocean triple junction is reduced by 40%. Australia and India are conventionally thought to be contained in a single plate divided from an Arabian plate by the Owen Fracture Zone. Continental Transform Faults: Congruence and Incongruence With Normal Plate Kinematics. The 2 March 2016 Wharton Basin M 7.8 earthquake: High stress drop north‐south strike‐slip rupture in the diffuse oceanic deformation zone between the Indian and Australian Plates. Journal of Geomagnetism and Aeronomy, Nonlinear Evaluation of seismic hazard in low to moderate seismic regions, Sri Lanka—a case study. This boundary, possibly initiated in late Miocene time, may be related to the opening of the Gulf of Aden and the uplift of the Himalayas.

/ Wiens, Douglas A.; DeMets, Charles; Gordon, Richard G.; Stein, Seth A; Argus, Don; Engeln, Joseph F.; Lundgren, Paul; Quible, Dan; Stein, Carol; Weinstein, Stuart; Woods, Dale F. T1 - A diffuse plate boundary model for Indian Ocean tectonics. Risk of fire occurrence in arid and semi-arid ecosystems of Iran: an investigation using Bayesian belief networks.

Plate motion inversions and an F‐ratio test show that relative motion data along the Carlsberg Ridge are fit significantly better by the new model. Gulf of Aden, and Red Sea"". We propose instead that … Effects of the heterogeneous subducting plate on seismicity: Constraints from b-values in the Andaman–Sumatra–Java subduction zone. We propose instead that motion along the nearly aseismic Owen Fracture Zone is negligible and that Arabia and India are contained within a single Indo‐Arabian plate, divided from the Australian plate by a diffuse boundary. Please check your email for instructions on resetting your password.

and Chemical Oceanography, Physical Spacing of faults at the scale of the lithosphere and localization instability: 2. in Modeling Earth Systems (JAMES), Journal of Geophysical Research This boundary, possibly initiated in late Miocene time, may be related to the opening of the Gulf of Aden and the uplift of the Himalayas.

The timing of uplift, volcanism, and rifting peripheral to the Red Sea: A case for passive rifting?. The anticorrelated velocities of Africa and India in the Late Cretaceous and early Cenozoic. Geophysics, Marine Lithospheric Deformation in the equatorial Indian Ocean: Timing and Tibet. Processes in Geophysics, Atmospheric Macrofracturing of Oceanic Lithosphere in Complex Large Earthquake Sequences. Cretaceous to present kinematics of the Indian, African and Seychelles plates, Slow-downs and speed-ups of India–Eurasia convergence since.

From what I understand it is when a plate collides with another plate, but it's not just a converging collision. It will have strike slips, and normal faults within it as well. A deterministic analysis of tsunami hazard and risk for the southwest coast of Sri Lanka. Plate motion inversions and an F‐ratio test show that relative motion data along the Carlsberg Ridge are fit significantly better by the new model. The misclosure of the Indian Ocean triple junction is reduced by 40%. We propose instead that motion along the nearly aseismic Owen Fracture Zone is negligible and that Arabia and India are contained within a single Indo‐Arabian plate, divided from the Australian plate by a diffuse boundary. These images show the locations of the plates … Oceanography, Interplanetary Uncertainties and implications of the Late Cretaceous and Tertiary position of North America relative to the Farallon, Kula, and Pacific Plates.

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