A non-local source for slate on the roof of Chingford Stables, Dunedin, New Zealand (note). [PDF]
Mortimer N +3 more
europepmc +1 more source
New Zealand's Second Meteorite: Makarewa (find, L4, S5, W2)
One of the most remarkable discoveries of a meteorite in New Zealand was that of Makarewa. Discovered in 1879, Makarewa is a ‘find’ that was uncovered a metre below the surface of a clay bank during excavation works for a train line in the southern South Island.
Mia R. E. Boothroyd +3 more
wiley +1 more source
Coupling antigorite deformation and dehydration in high-pressure experiments. [PDF]
Eberhard L +6 more
europepmc +1 more source
ABSTRACT The sediment signature of glacial erosion products exported from Hudson Strait to the Labrador Sea during Hudson Strait Heinrich (HS‐H) events is evaluated using four distinct proxies: paired δ18Ο and δ13C data on the carbonate fraction, εNd and U–Pb isotopes in the silicate fraction, the mineral composition of the <2 mm bulk sediment fraction,
John T. Andrews +3 more
wiley +1 more source
Silicon isotopic signatures of granitoids support increased weathering of subaerial land 3.7 billion years ago. [PDF]
Greber ND +5 more
europepmc +1 more source
Abstract Subduction initiation often begins with slow, forced convergence, switches “on” catastrophically as the slab collapses into the mantle, and then evolves to steady‐state, self‐sustained sinking that drives global plate movements. Numerical models suggest that the collapse phase implies sudden weakening of the plate interface.
Alissa J. Kotowski +3 more
wiley +1 more source
Thermal buffering-controlled temperature variation between Mg-Al-rich rocks and migmatites. [PDF]
March S, Hand M, Morrissey L, Kelsey D.
europepmc +1 more source
Metamorphic CO2 Production in Collisional Orogens: Petrological Constraints from Phase Diagram Modeling of Himalayan, Scapolite-bearing, Calc-silicate Rocks in the NKC(F)MAS(T)-HC system [PDF]
Chiara Groppo +3 more
openalex +1 more source
Crustal Structure Across the Okavango Rift, Botswana: The SEISORZ Wide‐Angle Seismic Experiment
Abstract The Okavango Rift Zone (ORZ) is an incipient continental rift in Botswana at the terminus of the Southwestern Branch of the East African Rift System. The lack of syn‐rift magmatism and tectonic processes overprinting pre‐rift structures provide an opportunity to investigate incipient‐stage rift processes and the role of pre‐existing structures
J. Pablo Canales +7 more
wiley +1 more source
Distribution of natural radioactivity in different geological formations and their environmental risk assessment in Malaysia. [PDF]
Seow SQ +2 more
europepmc +1 more source

