Results 161 to 170 of about 274,135 (269)
Iron-rich Smectite Formation in Subseafloor Basaltic Lava in Aged Oceanic Crust. [PDF]
Yamashita S +4 more
europepmc +1 more source
Abiotic formation of condensed carbonaceous matter in the hydrating oceanic crust. [PDF]
Sforna MC +5 more
europepmc +1 more source
Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust. [PDF]
Aulbach S +5 more
europepmc +1 more source
This site contains 25 questions on the topic of oceanic and continental crust, which covers the physical properties and features of the two crust types. This is part of the Principles of Earth Science course at the University of South Dakota.
Timothy Heaton
core
Anaerobic Fungi: A Potential Source of Biological H2 in the Oceanic Crust. [PDF]
Ivarsson M +3 more
europepmc +1 more source
Degassing-induced fractionation of multiple sulphur isotopes unveils post-Archaean recycled oceanic crust signal in hotspot lava. [PDF]
Beaudry P +5 more
europepmc +1 more source
Selected Physical and Geotechnical Properties of Loess in Wairarapa Valley, New Zealand
Loess up to 10 m thick covers marine terraces, old river aggradation terraces, and gentle hill country slopes in Wairarapa, New Zealand. In the drier eastern and southern parts of Wairarapa, the loess is subject to dry summer and autumn and wet winter and spring in most years.
Alan S. Palmer
wiley +1 more source
Building a Continental‐Scale Geodetic Network: The Plate Boundary Observatory (PBO)
Abstract The Plate Boundary Observatory (PBO) transformed the use of geodesy in North America to study crustal deformation and plate boundary processes by establishing a continental‐scale, standardized, open‐access geodetic network. Built and operated by UNAVCO between 2003 and 2018 as part of the National Science Foundation (NSF)‐funded EarthScope ...
Emily E. Zawacki +5 more
wiley +1 more source
The Earth's Greatest Porous Media
Abstract How deeply does modern meteoric water circulate into the continental crust? How deep is the Earth's Critical Zone (CZ), the top layer of the continental lithosphere that co‐evolves with the atmosphere, hydrosphere, and biosphere, extending from vegetation canopy down to fresh bedrock and the base of active groundwater circulation?
Ying Fan +3 more
wiley +1 more source

