Geophysical characteristics of the southern Mariana Trough, 11°50′N-13°40′N

Geophysical characteristics of the southern Mariana Trough, 11°50′N-13°40′N is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2000JGR...10516591M
P356DOI10.1029/2000JB900117

P2093author name stringFernando Martínez
Nathan Becker
Patricia Fryer
P2860cites workNew, improved version of generic mapping tools releasedQ97585688
Origin and development of marginal basins in the western PacificQ97999065
Magnetic and tectonic studies of the dueling propagating spreading centers at 20°40′S on the East Pacific Rise: Evidence for crustal rotationsQ104729189
Ridges and basins of the Tonga-Kermadec Island Arc SystemQ29400052
Global Sea Floor Topography from Satellite Altimetry and Ship Depth SoundingsQ54170893
Mid-Ocean Ridges: Fine Scale Tectonic, Volcanic and Hydrothermal Processes Within the Plate Boundary ZoneQ55933724
Sea-floor spreading as thermal convectionQ56136695
Geodetic observations of very rapid convergence and back-arc extension at the Tonga arcQ56235202
Spreading center terms and conceptsQ56874551
Evolution of backarc rifting: Mariana Trough, 20°-24°NQ57533670
Crustal control of ridge segmentation inferred from observations of the Reykjanes RidgeQ59029319
The curvature of Wadati-Benioff zones and the torsional rigidity of subducting platesQ59052813
Evidence from gravity data for focused magmatic accretion along the Mid-Atlantic RidgeQ59091517
Small non-overlapping offsets of the East Pacific RiseQ59096224
Subalkaline andesite from Valu Fa Ridge, a back-arc spreading center in southern Lau Basin: petrogenesis, comparative chemistry, and tectonic implicationsQ59810806
Deformation of a weak subducted slab and variation of seismicity with depthQ60067687
Twin active spreading ridges in the North Fiji Basin (southwest Pacific)Q61662774
Along-axis gravity gradients at mid-ocean ridges: Implications for mantle flow and axial morphologyQ61906107
Seismic slip and down-dip strain rates in wadati-benioff zonesQ81131632
Southern Mariana Arc: Geophysical Observations and Hypothesis of EvolutionQ96731971
P433issueB7
P407language of work or nameEnglishQ1860
P304page(s)16591-16607
P577publication date2000-07-10
P1433published inJournal of Geophysical ResearchQ2738009
P1476titleGeophysical characteristics of the southern Mariana Trough, 11°50′N-13°40′N
P478volume105

Reverse relations

cites work (P2860)
Q57873080A seismic stratigraphic analysis of Mariana forearc basin evolution
Q54087280An updated digital model of plate boundaries
Q29038772Asymmetric accretion along the slow-spreading Mariana Ridge
Q57870296Bathymetry of Mariana trench-arc system and formation of the Challenger Deep as a consequence of weak plate coupling
Q59792744Fore-arc basalts and subduction initiation in the Izu-Bonin-Mariana system
Q56806201Hydrothermal activity and volcano distribution along the Mariana arc
Q56771334Kinematics of subduction and subduction-induced flow in the upper mantle
Q57873043Malaguana-Gadao Ridge: Identification and implications of a magma chamber reflector in the southern Mariana Trough
Q42041874Mantle wedge control on back-arc crustal accretion
Q97455716Peridotites from a ductile shear zone within back-arc lithospheric mantle, southern Mariana Trench: Results of a Shinkai 6500 dive
Q57873073Sedimentary, volcanic, and tectonic processes of the central Mariana Arc: Mariana Trough back-arc basin formation and the West Mariana Ridge
Q29035882Spreading process of the northern Mariana Trough: Rifting-spreading transition at 22°N
Q57869223Stress field along the Ryukyu Arc and the Okinawa Trough inferred from moment tensors of shallow earthquakes
Q59418603Thermomechanical models for the dynamics and melting processes in the Mariana subduction system
Q57525915Three-dimensional visualization of a near-vertical slab tear beneath the southern Mariana arc
Q104150428Upper Plate Stress Controls the Distribution of Mariana Arc Volcanoes
Q57276162Why is the Challenger Deep so deep?

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