Serpentine and the subduction zone water cycle

By L. Rüpke, J. Morgan, M. Hort, J. A. Connolly. 2004

763 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/32221e287cae4d0eb51351835f67edaa814bcaf7

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In Geophysics

Citations in the corpus

Plate tectonics on the early Earth: Limitations imposed by strength and buoyancy of subducted lithosphere (2008, methodology): “Here, we examine this role by changing the (default) kinetics (full transition within 1 Ma) to 5 Ma (Figure 7). Rubie (1990) , Hacker (1996) and Austrheim (1998) showed that hydration is expected to influence the eclogitization dynamics significantly.”
The solid Earth’s influence on sea level (2013, methodology): “…stability of Earth’s surface reservoirs (Hirschmann, 2006), they are not inconsistent with ~0.2 m/m.y. of sea-level change if this change occurred fi rst as Archean degassing followed by Proterozoic regassing, as some models suggest (Maruyama and Liou, 2005; Rüpke et al., 2004; Sandu et al., 2011).”
Water, Melting, and the Deep Earth H 2 O Cycle (2006, background): “Thus, the fluxes of H2O into the deep mantle must be closely in balance with degassing at ridges and regassing at subduction zones (McGovern & Schubert 1989, Rüpke et al. 2004).”
A model for C-O-H fluid in the Earth's mantle (2009, background): “…fluid– rock interactions (McCollom and Shock, 1998; Zheng et al., 1999), dehydration of subducted slabs (Gerya and Yuen, 2003; Spandler et al., 2003; Rupke et al., 2004), destruction of craton (Liu, 2005), metasomatism (Stalder 0016-7037/$ - see front matter 2009 Published by Elsevier Ltd.…”
H2O subduction beyond arcs (2008, methodology): “These cycle times are compromised by variations in many parameters (including the rate of mantle degassing, rate of continental growth, spreading rates, average age of subducting slabs, and volume of subducting sediments [e.g., McGovern and Schubert, 2005; Jarrard, 2003; Rüpke et al., 2004]) over th”