FN Archimer Export Format
PT J
TI A Rosetta stone linking melt trajectories in the mantle to the stress field and lithological heterogeneities (Trinity ophiolite, California)
BT 
AF Ceuleneer, Georges
   Rospabé, Mathieu
   Chatelin, Tom
   Henry, Hadrien
   Tilhac, Romain
   Kaczmarek, Mary-Alix
   Le Sueur, Elisabeth
AS 1:1;2:2,3;3:1;4:1;5:4;6:1;7:5;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Géosciences Environnement Toulouse, Toulouse University, CNRS, IRD, 14 Avenue E. Belin, 31400 Toulouse, France
   Research Institute for Marine Geodynamics (IMG), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 Natsushima, Yokosuka, Kanagawa 237-0061, Japan
   Geo-Ocean, Univ Brest, CNRS, Ifremer, UMR6538, F-29280 Plouzané, France
   Instituto Andaluz de Ciencias de la Tierra (IACT), Consejo Superior de Investigaciones Científicas (CSIC)–Universidad de Granada, 18100 Armilla, Granada, Spain
   53 rue Fontaine des Cerdans, 31520 Ramonville, France
C2 UNIV TOULOUSE, FRANCE
   JAMSTEC, JAPAN
   Geo-Ocean, Univ Brest, CNRS, Ifremer, UMR6538, F-29280 Plouzané, France
   CSIC, SPAIN
   53 rue Fontaine des Cerdans, 31520 Ramonville, France
IF 5.8
TC 2
UR https://archimer.ifremer.fr/doc/00795/90728/96314.pdf
   https://archimer.ifremer.fr/doc/00795/90728/96315.zip
LA English
DT Article
AB Infiltration triggered by selective dissolution of pyroxenes is a major mode of melt migration in the mantle. A common view, supported by experiments and numerical models, is that the geometry of the melt plumbing system is governed by the stress field induced by solid-state flow of the host peridotite. Yet, salient melt migration structures frozen at an early stage of development in the mantle section of the Trinity ophiolite reveal that lithological heterogeneities drastically impact melt trajectories. Where melts reach a pyroxenite layer, dissolution-induced permeability abruptly increases, initiating a feedback loop confining melt migration to that layer regardless of its orientation relative to the stress field. This process results in the development of a network of interweaved dunitic channels evolving to thick tabular dunites where the melt reacts with closely spaced pyroxenite layers. This reacting melt was rich in alkali elements and water, as evidenced by the minerals (mostly amphibole and micas) encapsulated in the Cr-spinel grains that crystallized during the reaction. This “pioneer melt” differs from the volumetrically dominant depleted andesite that fed the crustal section. In fact, the migration of andesite benefited from the enhanced permeability provided by the dunites formed by the pioneer melt. As a result, dunites are palimpsests, the compositions of which record successive percolation events. The geometry of the melt pathways is extremely challenging to model because the abundance, spacing, and orientation of lithological heterogeneities cannot be predicted, being inherited from a long geological history. 
PY 2022
PD OCT
SO Geology
SN 0091-7613
PU Geological Society of America
VL 50
IS 10
UT 000886618100021
BP 1192
EP 1196
DI 10.1130/G50083.1
ID 90728
ER

EF