Thermobarometric studies on the Levack Gneisses: Footwall rocks to the Sudbury Igneous Complex [PDF]
Granulite and amphibolite facies gneisses and migmatites of the Levack Gneiss Complex occupy a zone up to 8 km wide around the northern part of the Sudbury Igneous Complex (SIC).
James, R. S. +2 more
core +1 more source
Climatic control on the location of continental volcanic arcs. [PDF]
Muller VAP +4 more
europepmc +1 more source
Geomechanical models of impact cratering: Puchezh-Katunki structure [PDF]
Impact cratering is a complex natural phenomenon that involves various physical and mechanical processes. Simulating these processes may be improved using the data obtained during the deep drilling at the central mound of the Puchezh-Katunki impact ...
Ivanov, B. A.
core +1 more source
Cooling rates and melt extraction timescales determined by diffusion chronometry on shallow crustal plutonic rocks. [PDF]
Grocolas T +5 more
europepmc +1 more source
Deep geothermal energy extraction can potentially reduce temperature and discharge at hot springs. [PDF]
Neupauer RM, Carter AJ, Ge S.
europepmc +1 more source
Geological sketch map and implications for ice flow of Thwaites Glacier, West Antarctica, from integrated aerogeophysical observations. [PDF]
Jordan TA +3 more
europepmc +1 more source
The Cretaceous-Tertiary (K/T) impact: One or more source craters? [PDF]
The Cretaceous-Tertiary (K/T) boundary is marked by signs of a worldwide catastrophe, marking the demise of more than 50 percent of all living species. Ever since Alvarez et al.
Koeberl, Christian
core +1 more source
Tectonism rather than "snowball Earth" glaciation is responsible for the Great Unconformity. [PDF]
Zhan RR +11 more
europepmc +1 more source
Thermochronologic constraints on the origin of the Great Unconformity. [PDF]
McDannell KT +4 more
europepmc +1 more source
Evolution of ancient hydrothermal fluids theoretically inverted with initial oxygen isotopes of water. [PDF]
Wei CS, Zhao ZF.
europepmc +1 more source

