Results 111 to 120 of about 105,881 (342)
Shallow‐marine mudstone of the Cretaceous Kaskapau Formation in the British Columbia foredeep preserves a 185 m thick record of OAE2. The organic carbon‐isotope and osmium‐isotope excursions can be correlated in detail with other Cenomanian–Turonian boundary sections around the world.
A. Guy Plint +12 more
wiley +1 more source
International Union of Geodesy and Geophysics: Rome Assembly, 1954 Meeting of The Commission on snow and Ice [PDF]
V. E. Fuchs
openalex +1 more source
This study integrates sedimentological and ichnological data to reveal the depositional processes and environmental conditions of deep‐water muddy gravity flows in the Mobarak Formation. It highlights distinct ichnocoenoses and bioturbation patterns, offering insights into basin‐floor versus slope mudstones and their implications for hydrocarbon ...
Aram Bayet‐Goll +2 more
wiley +1 more source
Controls on carbonate island formation and evolution: South Joulter Cay, Great Bahama Bank
The evolution of South Joulter Cay occurs in three stages: linear ridges shaped by waves and longshore currents, arcuate ridges influenced by tidal currents and channels, and cuspate ridges formed by variable wind and wave directions. These processes are driven by climatic and oceanographic factors.
Juan Carlos Laya +3 more
wiley +1 more source
Encyclopedia of Solid Earth Geophysics
H. Gupta
semanticscholar +1 more source
Our research uses a multidisciplinary approach, including organic and inorganic geochemistry, biostratigraphy, carbon isotope geochemistry and organic petrography to reconstruct depositional conditions and organic matter accumulation during the Pliensbachian and Toarcian.
Premila Wijesinghe +7 more
wiley +1 more source
Erratum: Significance of the Radioactivity of Potassium in Geophysics. II [PDF]
T. Gráf
openalex +1 more source

