Fig. 1 Volcanotectonic and chemical stratigraphy of the upper part of the OS of the BGB, with estimates of water depth. Volcanotectonic and chemical stratigraphy.

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Fig. 1 Volcanotectonic and chemical stratigraphy of the upper part of the OS of the BGB, with estimates of water depth. Volcanotectonic and chemical stratigraphy of the upper part of the OS of the BGB, with estimates of water depth. The left column shows tectonostratigraphy at the main shear zones (SZ; purple), and unconformity separating the HC (dark green; with the 10 main chert horizons HC1 to HC10 in dark gray) from its underlying complex (Komatii Complex; not marked), and the NC (yellow) from the KC (pale green) and the MC (orange), together with selected radiometric ages from the sequences [modified from de Wit et al. (18)]. Note that the HC is separated from the NC (yellow) by a major unconformity that cuts down from above HC10 to below HC6 [into eruption phase 5 (EP5)]. The two central columns show the δ18O and SiO2 values of the mafic volcanic rocks and of a few intrusive rocks of the HC and KC, as well as 6 of the 10 chert horizons of the HC (HC1 to HC10) that separate its nine eruption phases [EP1 to EP9, as defined in Furnes et al. (20); see also Fig. 2]. Note how the δ18O values in EP1 to EP4 and EP9 trend toward mantle values above and below their respective bounding chert bars (see text for further explanation). The δ18O and SiO2 values of the hydrothermal field site (on HC2), including the material of the hydrothermal pipes (red triangles), are also shown. For detailed sample sites, field relationships, geochemical data, and temperature calculations, see Figs. 2 to 5, tables S1 and S2, and figs. S1 to S3. Maarten J. de Wit, and Harald Furnes Sci Adv 2016;2:e1500368 Copyright © 2016, The Authors