Fig. 2: Longqi-1 hydrothermal vent fluids in comparison with vent fluid compositions from other vent sites. | Nature Communications

Fig. 2: Longqi-1 hydrothermal vent fluids in comparison with vent fluid compositions from other vent sites.

From: Deep high-temperature hydrothermal circulation in a detachment faulting system on the ultra-slow spreading ridge

Fig. 2

a Dissolved B versus chloride; b dissolved K/Cl versus Ca/Cl; c dissolved silicon versus chloride; d dissolved lithium versus chloride (see text). Data sources for mafic-hosted systems are as follows: EPR57,58,59,60,61; JdFR: ASHES62; Southern JdFR63; MEF28,64; MAR: TAG43,65,66; and Lucky Strike30. Other host lithologies on MAR: Rainbow67; Nibelungen (8˚18′S)29; Logatchev (14˚45′N)38; and Central Indian Ridge68 are displayed for comparison. All the error bars are smaller than the scale of the symbols.

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