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Fluid evolution in an Oceanic Core Complex: a fluid inclusion study from IODP hole U1309 D - Atlantis Massif, 30°N, Mid-Atlantic Ridge

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Figure

Figure 1. 3-D view of the Atlantis Massif showing morphotectonic features and the location of IODP holes U1309A-E
Figure 2. Schematic 3-D block diagram of the Atlantis Massif. Detachment fault is shown as a curved white line which steepens at depth.Location of U1309D is also shown in white
Figure 3. Photomicrographs; (a) ophitic texture of diabase with laths of plagioclase, green hornblende, and clinopyroxene relics as brightcolors (sample U1309D 16R-2 58–61 piece 4, cross-polarized light)
Table 1. Electron Microprobe Analyses of Plagioclases and Amphiboles in Diabase Sample U1309D 1R-1 41–44a
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