The life cycle of a continent is driven by the very dynamic lithosphere and asthenosphere system. The deformation associated with tectonic events, such as plate …
Upon hypervelocity impact, projectile and target materials are frequently shocked to pressures and temperatures sufficient to induce complete vaporization. Vaporization associated with impacting comets and …
Policy and practice in major river systems of the world continue to degrade ecosystems and undermine sustainable use. Freshwater resources are multi-valued, and transboundary river …
Why are the planets of our Solar System so different, geologically? Volcanic, tectonic, and magnetic processes are responsible for many important features of the Earth, …
Asteroids and their meteoritic counterparts are the most accessible, yet most enigmatic solar system materials available for study. Their chemistry and mineralogy provide clues to …
The three-dimensional distribution of materials within the lunar crust is a source of information about the thermal and structural history of the Moon. Patterns observed …
This work is perhaps the first major study integrating mineralogical and morphological properties of lunar impact melt deposits using the new generation remote sensing data. …
Detailed textural, mineralogical and chemical analyses of extraterrestrial materials have raised numerous questions about the igneous evolution and cooling histories of their parent bodies. Remote …
The thermohaline instabilities imposed by sea ice floes on the surface ocean create submesoscale eddies which are poorly modelled in modern oceanographic or atmospheric models. …
The state of the climate during the Late Noachian/Early Hesperian has been a longstanding question in Mars research. The abundant fluvial features and alteration minerals …
Reactive nitrogen gases (e.g., NOx = NO + NO2) emitted to the atmosphere eventually return to the surface environment as nitrate (NO3-) deposition, which causes …
The lithosphere preserves a record of tectonic evolution in its seismic velocity structure, reflecting variations in temperature, composition, and physical state. However, individual seismic observations …
Partial melting of the mantle occurs predominantly in the spinel lherzolite stability field, where pyroxenes are consumed to produce olivine and basaltic melt. The phase …
Over the past four decades, the Cerrado region of Brazil has transitioned from a land of sparsely inhabited forests and shrublands to an industrial agriculture …
Ocean surface gravity waves, especially the resulting Langmuir turbulence, affect the ocean surface vertical mixing, yet are missing in most of the global climate models …
The Indian Summer Monsoon (ISM) is vital to over one-fifths of the world’s population who depend upon monsoonal rains. Recently collected marine sediment cores offer …
This work presents novel Miocene – Pliocene (13 - 2.6 Ma) sea surface temperatures (SST) from the Mediterranean Sea, North Atlantic, South Atlantic and North …
The Pliocene epoch (5.33-2.58 million years ago, Ma) has relevance to understanding Earth’s modern climate, as it is the most recent time in Earth’s history …
Seismic anisotropy in olivine and orthopyroxene mineral crystals enables us to infer first-order flow characteristics in the asthenospheric mantle and the preserved tectonic history in …