Abstract
Rare gases are conservative tracers of subsurface fluid movement. The mass balance of atmosphere-derived and crustally produced radiogenic and nucleogenic rare gases in natural gas reservoirs allows straightforward constraints to be placed on scales of fluid movement in sedimentary basins. The details of large-scale fluid movements in Neogene sedimentary basins appear to differ according to their thermal structures.
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Schedule a callMore From: Philosophical Transactions of the Royal Society of London. Series A: Physical and Engineering Sciences
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