Results 131 to 140 of about 1,726,480 (235)
Middle-late Devonian warming and land plant evolution drive changes in silicate weathering: A new 87Sr/86Sr conodont record paired with δ18O [PDF]
The Devonian Period (419 to 359 Ma) is marked by a shift from cooling in the Early Devonian to warming in the Middle-Late Devonian. Previous studies have hypothesized that an increase in metamorphic degassing during the Acadian Orogeny caused the late ...
Mills, B.J.W. +4 more
core +1 more source
Abstract The rarity of natural rocks that specifically record the physicochemical conditions of the subduction interface strongly hampers pertinent studies on metamorphic trajectories of high‐pressure (HP) rocks and related fluid–rock interactions. This study examines an oceanic eclogite block from the Huwan shear zone in the Hong'an orogen.
Dadi Cao +4 more
wiley +1 more source
Abstract Ophiolitic mélanges and associated intrusions provide key archives for reconstructing the evolution of ancient ocean basins and subduction‐related mantle modification. The Hongliuhe–Niujuanzi–Xichangjing ophiolitic mélange in the central Beishan Orogen preserves important records of the Paleo‐Asian Ocean, but the timing of oceanic subduction ...
Yujia Song +4 more
wiley +1 more source
The Devonian continental rocks of the lower Restigouche River, Quebec
The Devonian continental rocks outcropping between Campbellton, New Brunswick and Miguasha, Quebec are regrouped on the basis of new stratigraphic information and the ages now suggested are thought to be in accord with new data. An Early or early Middle
B. P. J. Williams, D. L. Dineley
core +1 more source
Abstract The paleogeographic position of the South China Block (SCB) during the early Paleozoic and its affiliation with Gondwana remain debated. We report new high‐quality paleomagnetic data from sandstone‐dominated Cambrian Stage 3 strata correlated with the Yu'anshan–Hongjingshao succession collected along the southwestern margin of the SCB ...
Dongmeng Zhang +14 more
wiley +1 more source
Abstract Following continental collision, the distal European margin was overridden by the Alpine wedge and is now largely concealed beneath the mostly intact orogenic lid. Consequently, the geological evolution and nature of the hidden basement domains remain poorly constrained.
Bianca Heberer +11 more
wiley +1 more source
A provisional Radiolaria biostratigraphy, Late Devonian through Late Permian [PDF]
Brian K. Holdsworth +1 more
openaire +1 more source
The walls boundary fault zone and the MØre TrØndelag fault complex:: a case study of two reactivated fault zones. [PDF]
It is commonly observed that ancient faults or shear zones can become reactivated again and again, either within the same or even superimposed tectonic episodes, yet millions of years apart.
Watts, Lee Mark
core
Abstract Detrital zircon U–Pb geochronology from Triassic–Jurassic basins in the New England Orogen (NEO) constrains sediment provenance and episodic continental arc evolution along the eastern Gondwanan margin. Dominant zircon clusters at 270–230 Ma and 340–300 Ma in these basins were likely sourced from contemporaneous magmatism in the NEO ...
Yanxiong Zhang +2 more
wiley +1 more source
Temperate semi‐natural grasslands soil organic carbon (SOC) stock was significantly associated with soil characteristics, climate, vegetation structure and management. These results indicate that maintaining long‐term extensive management and preventing conversion or degradation of semi‐natural grasslands can simultaneously support biodiversity ...
Elvi Liiv, Triin Reitalu, Aveliina Helm
wiley +1 more source

