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406.01 - Leslie Rogers -- How Many Exoplanets Does it Take to Constrain the Origin of Mercury?
It is a key region to constrain the origin of the deep-water basins and intervening ridges of the Amerasia Basin.
We find that the stable carbon isotope data do not constrain the origin of the dissolved CO2 in the Kerr groundwaters.
Chemical and isotopic compositions of bubbling gases were analyzed to constrain the origin of the gases emitted through the water of Katanuma lake.
More stations are required to better characterize meteors and constrain the origin of the seismic signal source [e.g., Ishihara et al. (2004); Edwards et al. (2008); Heimann et al. (2013); Tauzin et al. (2013)].
In their second series of experiments, Hamada and Fujii (2007) conducted hydrous melting experiments on two drilling core samples of volcanic rocks from the Izu-Oshima volabeledlaseled as MA43 and MA44 (MgO approximately 5 wt.%; Additional file 2: Table S2), to constrain the origin of Ca-rich plagioclase.
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This study highlights the difficulty in constraining the origin of sustained turbidity currents in ancient sedimentary sequences.
These simulations allow us to find the shape of the magnetosphere and the location of particle acceleration regions, constraining the origin of high energy emission.
Fossil evidence constrains the origin of the geophagine genus Gymnogeophagus to a conservative estimate of at least 39.9 million years old, although it is likely older [ 9, 59, 60].
For these eight loci, we ran the divergence time analyses multiple times with various parameters, including enforcing a constraint of 210 330 Ma for the origin of teleost paralogs, and when data were available for the gar, we constrained the origin of neopterygians (gars, bowfins, and teleosts) to a minimum of 141 Myr based on the oldest lepisosteid fossil (from the Cretaceous, Gardiner 1993).
We further constrain the lithologic origin of the plagioclase-rich lithic fragments based on the range of crystallization ages reported for different lithologic components (Table 3).
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