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Temporal changes in the geomagnetic field termed secular variation (SV) may provide constraints on the fluid dynamics at the top of the core and possibly on the dynamo action.
This provides us with evidence of natural carbon cycle sensitivity to climate, and may provide constraints on future feedbacks in response to long-term climate change.
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Therefore, resistivity anomalies may provide critical constraints leading to better models of hydrothermal systems.
Improved observations, in particular higher quality planetary magnetic field models, may provide tighter constraints on the dynamo models.
For the presence of anelastic attenuation and anisotropic symmetries, these relations may provide improved constraints on thermal/compositional structure and deformational processes in the interior of Earth.
Our combined approach may provide new constraints on the organization of magma plumbing systems beneath volcanoes in continental and marine settings.
Second, individuals are not bounded, isolated beings, but part of families and social networks (whether nearby or in country of origin) that may provide both constraints and opportunities across each integration domain.
In particular, simultaneous observations of subsurface and surface phenomena may provide strong constraints on magma plumbing systems and eruption column dynamics, furthering insight of the mechanisms of diverse eruption styles.
The spatial distribution of lithospheric rheology structure may provide important constraints on understanding of intra- or inter-plate deformation mechanism, and more studies are needed to further understand the tectonic process es) accompanying different lithosphere rheology structures.
This approach appears promising for characterizing temporal changes in mouse models of human neurological and psychiatric conditions, and may provide anatomical constraints for other preclinical imaging, e.g. fMRI and molecular imaging.
More broadly, we find that excess barium coupled with redox proxies may provide useful constraints on the interplay between preservation and production controls on organic matter abundances in the Paleozoic successions.
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