Journal Title |
Article Title |
Year |
DOI |
Chinese Journal of Oceanology and Limnology
|
Trace element composition of peridotites from the southern Mariana forearc: Insights into the geochemical effects of serpentinization and/or seafloor weathering |
2009
|
10.1007/s00343-009-9252-6
|
International Journal of Earth Sciences
|
Mineral chemistry and geochemistry of ophiolitic metaultramafics from Um Halham and Fawakhir, Central Eastern Desert, Egypt |
2018
|
10.1007/s00531-018-1601-2
|
Geochemistry, Geophysics, Geosystems
|
Variability in serpentinite mudflow mechanisms and sources: ODP drilling results on Mariana forearc seamounts |
2006
|
10.1029/2005GC001201
|
Geoscience Frontiers
|
Geochemistry of subducted metabasites exhumed from the Mariana forearc: Implications for Pacific seamount subduction |
2021
|
10.1016/j.gsf.2020.12.002
|
Journal of Petrology
|
Geochemistry of Ocean Floor and Fore-arc Serpentinites: Constraints on the Ultramafic Input to Subduction Zones |
2012
|
10.1093/petrology/egr058
|
Geochimica et Cosmochimica Acta
|
Isotopic and element exchange during serpentinization and metasomatism at the Atlantis Massif (MAR 30°N): Insights from B and Sr isotope data |
2008
|
10.1016/j.gca.2008.01.013
|
Annual Review of Marine Science
|
Serpentinite Mud Volcanism: Observations, Processes, and Implications |
2012
|
10.1146/annurev-marine-120710-100922
|
Journal of Geophysical Research: Solid Earth
|
Shallow slab fluid release across and along the Mariana arc‐basin system: Insights from geochemistry of serpentinized peridotites from the Mariana fore arc |
2007
|
10.1029/2006JB004749
|
Journal of Earth System Science
|
Geochemistry of abyssal peridotites from the super slow-spreading Southwest Indian Ridge near 65°E: Implications for magma source and seawater alteration |
2012
|
10.1007/s12040-012-0229-z
|
Chemical Geology
|
In situ characterization of serpentinites from forearc mantle wedges: Timing of serpentinization and behavior of fluid-mobile elements in subduction zones |
2010
|
10.1016/j.chemgeo.2009.10.002
|