Results 51 to 60 of about 799 (197)
The enrichment and geochemical significance of elements associated with Late Permian coals in Southwest China have always gained widespread interest in the field of coal geology.
Shenjun Qin +4 more
doaj +1 more source
Extremely reducing conditions reached during basaltic intrusion in organic matter-bearing sediments [PDF]
International audienceRedox conditions in magma are widely interpreted as internally buffered and closely related to that of their mantle source regions.
Arndt, Nicholas +6 more
core +3 more sources
Tectonic Settings of Magmatic Sulfide Deposits in China [PDF]
published_or_final_versio
Keays, RR, Lesher, CM, Song, X, Zhou, MF
core
Palaeogeothermal response and record of the effusing of Emeishan basalts in the Sichuan basin
Thermal history of the Sichuan basin is reconstructed based on vitrinite reflectance from boreholes in the basin using a paleo-heat flow method. The results show that the Sichuan basin experienced a relatively low heat flow period in the Early Paleozoic, and an elevated paleo-heat flow, ranging 60∼80 mW/m2 with a maximum as high as 100 mW/m2 around 259
ChuanQing Zhu +7 more
openaire +1 more source
Chemical heterogeneity of the Emeishan mantle plume: Evidence from highly siderophile element abundances in picrites [PDF]
Highly magnesian lavas or picrites have the potential to preserve important information about the origin and thermochemical state of the mantle source(s) of large igneous provinces.
Ali +92 more
core +2 more sources
Numerical Modeling of Purely Active (Plume‐Produced) Continental Rifting and Break‐Up
Abstract In contrast to the traditional mechanism of passive continental rifting (driven by far‐field tectonic forces), the active rifting‐to‐break‐up processes (caused by rising mantle plumes) are still poorly understood. However, most episodes of fragmentation of the last supercontinent Pangea were relatively shortly preceded (within ∼10 Myr) by the ...
Alexander Koptev +12 more
wiley +1 more source
The link between mantle plumes and the formation of large igneous provinces (LIPs) is well established although the anatomy of these remains equivocal. Recent experimental studies and geophysical data suggest that the mantle plume head is more likely to ...
Hongbo Li +9 more
doaj +1 more source
[Purposes] The ore concentration area in northeast Yunnan is an important part of the Sichuan-Yunnan-Guizhou polymetallic metallogenic domain. Even in the extensively studied Huize Pb-Zn deposit in the area, the source of ore-forming materials is still ...
ZHANG Yan +3 more
doaj +1 more source
Abstract Thermomagnetic susceptibility (κ‐T) curves are used widely for magneto‐mineralogical analysis. Humps in heating curves below the Curie temperature of magnetite are observed frequently. We present κ‐T curves with hump features in magnetite‐bearing flood basalt samples.
Qi Zhang +5 more
wiley +1 more source
Abstract Viscosity of silicate melts governs magma transport and influences mantle dynamics, yet effects of pressure and water on melt viscosity remain poorly understood. Here, we report in situ falling‐sphere viscosity measurements on diopside (Di) melts with 0–3 wt.% H2O along the liquidus up to 7 GPa and 2103 K using synchrotron X‐ray radiography ...
Qi Chen +4 more
wiley +1 more source

