Identification of mantle plumes in the Emeishan Large Igneous Province
The plume hypothesis has been recently challenged largely because some fundamental aspects predicted by the modeling of plumes are found to be lacking in some classic hotspot regions. This review paper summarizes recent achievements made in the late Permian Emeishan continental flood basalt province in southwest China. Data from various disciplines are
Xu, Yi-Gang +10 more
openaire +2 more sources
Magnetostratigraphic constraints on two‐stage eruptions of the Emeishan continental flood basalts [PDF]
Temporal and spatial variations of high and low contents of Ti basalts in the Permian Emeishan large igneous province (ELIP) of southwest China and Vietnam are crucial for modeling of continental basalt formation and the nature of mantle‐lithosphere interaction.
Liandi Zheng +3 more
openaire +1 more source
The accurate identification of host mineral and the formation stage of fluid inclusions are critical to temperature measurement, and the combination of inclusion technology and other technologies could be better to figure out the source and properties ...
LAN Ye-fang +4 more
doaj +1 more source
A geomagnetic polarity timescale for the Permian, calibrated to stage boundaries [PDF]
The reverse polarity Kiaman Superchron has strong evidence for at least three, or prob ably four, normal magnetochrons during the early Permian. Normal magnetochrons are during the early Asselian (base CI1r.1n at 297.94+0.33 Ma), late Artinskian (CI2n at
Balabanov, Yuri P. +1 more
core +1 more source
The Emeishan large igneous province (hereafter named by its acronym ELIP) is the first accepted large igneous region in China. The current study tries to reconstruct the density structure of the crust in this region.
Xi Zhang +5 more
doaj +1 more source
New insights into the petrogenesis of the Jameson Range layered intrusion and associated Fe-Ti-P-V-PGE-Au mineralisation, West Musgrave Province, Western Australia [PDF]
The Mesoproterozoic Jameson Range intrusion forms part of the Giles Complex, Musgrave Province, Western Australia. It is predominantly mafic in composition comprising olivine-bearing gabbroic lithologies with variable amounts of magnetite and ilmenite ...
Gutzmer, Jens +4 more
core +1 more source
Early Cretaceous high-Ti and low-Ti mafic magmatism in Southeastern Tibet: Insights into magmatic evolution of the Comei Large Igneous Province [PDF]
The Dala diabase intrusion, at the southeastern margin of the Yardoi gneiss dome, is located within the outcrop area of the ~ 132 Ma Comei Large Igneous Province (LIP), the result of initial activity of the Kerguelen plume.
Antoshechkina, Paula M. +8 more
core
Abstract The southeastern Tibetan Plateau (SETP) plays a pivotal role in accommodating intra‐continental deformation driven by the ongoing India‐Eurasia convergence. However, its contemporary surface vertical motions and the underlying geodynamic processes remain highly debated.
Lei Liu +8 more
wiley +1 more source
Heavy boron isotopes in plume-derived magmas trace recycled water in deep-mantle reservoir
The debate on the origin of water in the Earth’s interior focuses on whether it originates from internal primordial sources or externally from the Earth’s surface via subduction-related processes. Here we report boron isotope data for Middle/Late Permian
Jian Xu +10 more
doaj +1 more source
In-domain control of a heat equation: an approach combining zero-dynamics inverse and differential flatness [PDF]
This paper addresses the set-point control problem of a heat equation with in-domain actuation. The proposed scheme is based on the framework of zero dynamics inverse combined with flat system control.
Zheng, Jun, Zhu, Guchuan
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