Results 201 to 210 of about 139,127 (283)
Beetle Pollination of Cycads in the Mesozoic
Chen-yang Cai +5 more
semanticscholar +1 more source
Abstract The High Arctic Large Igneous Province (HALIP) formed in the circum‐Arctic during the Cretaceous. The timing and duration of emplacement of these mafic magmas are important for understanding the climatic and environmental effects, yet many uncertainties remain. The dating methods used vary greatly between different regions.
A. M. R. Sartell +4 more
wiley +1 more source
New data concerning the age of Mesozoic limestone from Scarisoara (Bihor Mountains)
Ioan I. Bucur, Bogdan P. Onac
openalex +2 more sources
Seismic Insight on Basement Structure of the Extinct Mid‐Oceanic Ridge in Canada Basin, Arctic Ocean
Abstract The most accepted theory for the formation of the Canada Basin is that it was created during 66° rotation of Arctic Alaska around the Euler pole located near the Mackenzie Delta sometime during the Mesozoic. Gravity and magnetic anomaly data are consistent with an extinct mid‐oceanic ridge (MOR) in the central basin.
W. S. Priyanto, B. J. Coakley
wiley +1 more source
The Magmatic Plumbing System for Mesozoic High-Mg Andesites, Garnet-bearing Dacites and Porphyries, Rhyolites and Leucogranites from West Qinling, Central China [PDF]
Biji Luo +9 more
openalex +1 more source
Abstract Magmatic intrusions in rifted continental margins play a critical role in shaping structural evolution, yet their geometry and emplacement mechanisms remain poorly constrained in salt‐influenced terrains. The Moroccan Central High Atlas, a segment of the Atlas fold‐and‐thrust belt, hosts extensive Middle Jurassic to Early Cretaceous intrusions
Naheem Banji Salawu +5 more
wiley +1 more source
Characteristics of ∼40 Ma Mafic Rocks in North Tibet and Their Tectonic Implications
Abstract Several magmatic belts are present in the Tibetan Plateau. Among these, the Qiangtang magmatic belt in North Tibet remains elusive. In particular, the petrogenesis, magma source, and tectonic implications of the ultramafic to mafic rocks in the North Qiangtang area are underinvestigated due to their sparsity and remoteness.
Shifeng Wang +3 more
wiley +1 more source

