This chapter is intended to give an overview on the fundamental concepts behind the
processes of magma mixing, broadly considering interactions between different magmas …

Climate change and complex anthropogenic activities have raised significant concerns
regarding Precipitation-Runoff Relationships (PRR). Traditional methods, assuming …

The principle of maximum entropy can provide consistent basis to analyze water resources
and geophysical processes in general. In this paper, we propose to assess the space-time …

Neoarchean hybrid granitoids from the Vila União suite are located in the central portion of
the Canaã dos Carajás domain, Carajás Province (Amazonian craton, Brazil), and suggest …

Variations in rainfall are a significant characteristic of semi-arid climates, and it is expected
that climate change will increase this variability in many such regions. To effectively plan …

Anthropogenic activities pose significant threats to hydrological regimes, leading to water
resource exhaustion through intensive streamflow consumption. To identify regions where …

Fluid mixing usually involves the interplay between advection and diffusion, which together
cause any initial distribution of passive scalar to homogenize and ultimately reach a uniform …

The mixing of magmas is a fundamental process in the Earth system causing extreme
compositional variations in igneous rocks. This process can develop with different intensities …

The rates and timescales of crustal magma transfer, storage, emplacement, and eruption are
a key to understanding subvolcanic processes, characterizing volcanic hazards, and …

The Shannon entropy is a rigorous measure to evaluate the complexity in dynamical
systems. Shannon entropy can be directly calculated from any set of experimental or …