Site U1496

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[3]  C. G. Wheat,et al.  Expedition 366 summary , 2018 .

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[5]  G. Moore,et al.  Pacific Plate subduction beneath the central Mariana and Izu‐Bonin fore arcs: New insights from an old margin , 2008 .

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[7]  Alistair Black,et al.  Introduction , 2004, Libr. Trends.

[8]  M. Mottl,et al.  Deep‐slab fluids fuel extremophilic Archaea on a Mariana forearc serpentinite mud volcano: Ocean Drilling Program Leg 195 , 2003 .

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[10]  K. Horai,et al.  Heat Flow Measurements on Deep Sea Drilling Project Leg 60 , 1982 .

[11]  A. Despairies Authigenic Minerals in Volcanogenic Sediments Cored during Deep Sea Drilling Project Leg 60 , 1982 .

[12]  J. C. Jaeger The effect of the drilling fluid on temperatures measured in bore holes , 1961 .

[13]  J. Jaeger Conduction of Heat in an Infinite Region Bounded Internally by a Circular Cylinder of a Perfect Conductor , 1956 .

[14]  E. C. Bullard,et al.  The Time Necessary for a Bore Hole to Attain Temperature Equilibrium , 1947 .

[15]  T. Williams,et al.  International Ocean Discovery Program Expedition 366 Preliminary Report , 2017 .

[16]  T. Eglinton,et al.  8.6 – Organic Matter in the Contemporary Ocean , 2014 .

[17]  P. Fryer Serpentinite mud volcanism: observations, processes, and implications. , 2012, Annual review of marine science.

[18]  A. Oakley A multi-channel seismic and bathymetric investigation of the central Mariana convergent margin , 2008 .