Results 141 to 150 of about 14,501 (240)

Sequence stratigraphy of the syn-rift miocene succession in the Abu Rudeis-Sidri Field, Gulf of Suez, Egypt. [PDF]

Sci Rep
Assal EM, Farouk S, Omran MA, Belal N, Sarhan MA.   +4 more
europepmc   +1 more source

Giant Porphyry Copper Deposits Caused by a Slab Jamming in the Mantle Transition Zone

Terra Nova, Volume 38, Issue 2, Page 106-115, April 2026.
ABSTRACT Two giant porphyry copper deposits in the Southern Central Andes formed during the Miocene–Pliocene transition when a bend in the subducting Juan de Fernández hotspot chain jammed in the mantle transition zone, causing mega‐scale slab‐kinking. This geometry implies mechanical resistance that caused East–West compression and eventually a thrust‐
Nipaporn Nakrong, Marnie Forster, Wim Spakman, Hielke Jelsma, Francois Gaboury, Gordon Lister   +5 more
wiley   +1 more source

Remarkable dominance of myctophid otoliths in Upper Miocene Chagres Formation, Caribbean Panama. [PDF]

PeerJ
Lin CH, O'Dea A.
europepmc   +1 more source

3D Quantification of Subsidence During Pyrenean Retro‐Wedge Initiation: Role of Structural and Thermal Inheritance on Hyperextended Margin Inversion (Aquitaine Basin)

Terra Nova, Volume 38, Issue 2, Page 130-140, April 2026.
ABSTRACT We present novel 3D subsidence data enabling vertical movements' quantification during the early formation of the Pyrenean retro‐wedge. From Cenomanian to Turonian times, subsidence is relatively low (~26 ± 10 m/Myr), corresponding to a brief 10 Myr thermal re‐equilibration of the European lithosphere following the hyperextended rift episode ...
Benoit Issautier, Nicolas Saspiturry, Paul Angrand, Eric Lasseur, Simon Andrieu, Cécile Robin   +5 more
wiley   +1 more source

Late Miocene Arctic warmth and terrestrial climate recorded by North Greenland speleothems. [PDF]

Nat Geosci
Moseley GE, Koltai G, Baker JL, Wang J, Stoll H, Donner A, Friedrich L, Spötl C, Smith MP, Scholz D, Cheng H, Hartland A, Hejny C, Edwards RL.   +13 more
europepmc   +1 more source

Teleseismic Radial Anisotropy Reveals a Sill‐Dominated Magma Reservoir Beneath the Valles Caldera, New Mexico

Geophysical Research Letters, Volume 53, Issue 6, 28 March 2026.
Abstract The Valles Caldera (VC), one of the largest Quaternary silicic calderas in North America, formed by explosive rhyolitic eruptions. Seismic studies suggest a crustal magmatic reservoir beneath the caldera with low‐velocity anomalies, but resolving the detailed geometry of localized melt requires constraints from seismic anisotropy.
Gaoshan Guo, Haiqiang Lan, Tao Xu, Qinya Liu   +3 more
wiley   +1 more source

Global environmental drivers shape Cenozoic neoselachian diversity and identify modern conservation priorities. [PDF]

Sci Rep
Staggl MA, Villalobos-Segura E, Benton MJ, Kriwet J.   +3 more
europepmc   +1 more source

New Constraints on the Calabrian Arc (Central Mediterranean) Geodynamics: High‐Resolution Imaging of Lithospheric and Upper Mantle Discontinuities From P and S Receiver Functions

Geophysical Research Letters, Volume 53, Issue 6, 28 March 2026.
Abstract The Calabrian Arc subduction system (Central Mediterranean) is characterized by a deep and narrow (200 km) slab. Addressing the poorly understood link between shallow and deep mantle structures, we present the first high‐resolution mapping of crustal and upper mantle discontinuities across the Calabrian Arc and Southern Tyrrhenian basin.
C. Montuori, S. Monna, F. Frugoni, C. Piromallo, M. De Caro, A. Giuntini, A. Argnani   +6 more
wiley   +1 more source

Evolutionary genomics and divergence of Cacopsylla species with a special focus on the apple proliferation vectors Cacopsylla melanoneura and Cacopsylla picta. [PDF]

BMC Genomics
Ragionieri L, Serbina LŠ, Corretto E, Howie JM, Cruz F, Alioto TS, Zadra N, Weil T, Anfora G, Stauffer C, Ometto L, Rota-Stabelli O, Schuler H.   +12 more
europepmc   +1 more source

Two‐Stage Dolomite Formation in Carbonate Platforms Revealed by Carbonate Clumped Isotope Thermometry

Geophysical Research Letters, Volume 53, Issue 5, 16 March 2026.
Abstract The “dolomite problem” refers to the scarcity of dolomite in Cenozoic marine environments compared with its abundance in earlier strata. This discrepancy has been attributed to changes in marine environments or to insufficient thermal maturity required for dolomite formation.
Y. Levenson, J. M. Eiler, E. Wurgaft, N. Neagu, Y. Ebert, U. Ryb   +5 more
wiley   +1 more source