Results 211 to 220 of about 104,630 (326)
Abstract During the early Cenozoic greenhouse period, counterintuitive contractions in tropical Pacific oxygen‐deficient zones have been linked to enhanced deep‐ocean ventilation, yet direct geological evidence remains limited. Here we present molybdenum (Mo) isotopic records from International Ocean Discovery Program Site U1509.
Xiaowen Liu +8 more
wiley +1 more source
Redox state of subducted sediments controls porphyry copper mineralization along the Tethyan belt. [PDF]
Li H, Yang Z, Lu Y, Hou Z.
europepmc +1 more source
Albitization of feldspars in sandstones from the Upper Mesozoic Myogog Formation, Korea
Kang‐Min Yu +2 more
openalex +2 more sources
Two new caenogastropod genera from the Late Triassic Cassian Formation [PDF]
Nützel, Alexander
core +1 more source
Abstract Ocean bottom pressure recordings are a key observation for both ocean circulation and seafloor geodesy. New self‐calibrating instruments may solve a long‐time issue of instrument drift, allowing new high precision observations. However, instruments on the seafloor may settle over days to months, potentially contaminating results.
Nicholas Harmon +8 more
wiley +1 more source
Intraplate deformation of Gondwana terranes and implications for the Wilson Cycle. [PDF]
Fonseca A, De Grave J.
europepmc +1 more source
Abstract In 2022–2023, three local‐magnitude (ML) 4.8–5.6 earthquakes shook the Peace River oilsands area of Alberta, Canada. Previous studies statistically linked the seismicity to nearby disposal activities but lacked in‐depth investigation into triggering mechanisms, including subsurface fluid migration and earthquake interaction.
Wenhan Sun +10 more
wiley +1 more source
Protracted circum-continent subduction: A mechanism for craton destruction and a rationale for craton longevity. [PDF]
Xu X +12 more
europepmc +1 more source
Stochastic Resonance Elucidates the Emergence and Periodicity Transition of Glacial Cycles
Abstract Glacial cycles emerged with a 41‐kyr period after the Pliocene and later intensified with a 100‐kyr period in the mid‐Pleistocene, which were attributed to Earth's orbital variations. However, no significant changes in the orbital forcing were found at the two transitions, and the forcing was too small to drive these cycles. Here, a stochastic
Tian Xu, Gabriel Katul, Shineng Hu
wiley +1 more source

