about
A serpentinite-hosted ecosystem in the Southern Mariana ForearcVariability in serpentinite mudflow mechanisms and sources: ODP drilling results on Mariana forearc seamountsThree-dimensional visualization of a near-vertical slab tear beneath the southern Mariana arcCollisional model for rapid fore-arc block rotations, arc curvature, and episodic back-arc rifting in subduction settingsFormation mechanism of the moniliform seamounts outside the West Melanesian TrenchSeismicity and structure in central Mexico: Evidence for a possible slab tear in the South Cocos plateBathymetry of Mariana trench-arc system and formation of the Challenger Deep as a consequence of weak plate couplingMalaguana-Gadao Ridge: Identification and implications of a magma chamber reflector in the southern Mariana TroughSedimentary, volcanic, and tectonic processes of the central Mariana Arc: Mariana Trough back-arc basin formation and the West Mariana Ridge
P2860
Q28731748-FC467E17-13C1-465A-A85D-79BC52CA4FE4Q54087746-2F5247E8-46F9-497A-AEBF-282495BF9428Q57525915-F7388C6E-3471-45E5-9D57-C0D6FA36E97DQ57533672-566DE08F-49BD-425F-9265-EB980AC1E5B6Q57854534-68FC86D0-A32D-4E7E-9827-782DDF9DBB7BQ57869301-976A1F7A-835F-45E1-BFDD-7E7E850B4E40Q57870296-AC56F6B1-FCC6-4824-8309-7BC487B17F5DQ57873043-79F5C6A0-400B-4CE0-A610-4EFFC3AFA7F4Q57873073-745C8500-99F1-49A3-AD30-65C61A31BDC8
P2860
description
im Juni 2003 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в червні 2003
@uk
name
Why is the Challenger Deep so deep?
@en
Why is the Challenger Deep so deep?
@nl
type
label
Why is the Challenger Deep so deep?
@en
Why is the Challenger Deep so deep?
@nl
prefLabel
Why is the Challenger Deep so deep?
@en
Why is the Challenger Deep so deep?
@nl
P2093
P1476
Why is the Challenger Deep so deep?
@en
P2093
Bruce Appelgate
Fernando Martinez
Gerard Fryer
Margo Edwards
Nathan Becker
Patricia Fryer
P304
P356
10.1016/S0012-821X(03)00202-4
P407
P577
2003-06-01T00:00:00Z