[HTML][HTML] Layered intrusions: Fundamentals, novel observations and concepts, and controversial issues
Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
Rejuvenation of ancient micro-continents during accretionary orogenesis: Insights from the Yili Block and adjacent regions of the SW Central Asian Orogenic Belt
Abstract In the Central Asian Orogenic Belt (CAOB), whether substantial juvenile additions
associated with accretionary orogenesis are preserved is still a pending issue. The Yili Block …
associated with accretionary orogenesis are preserved is still a pending issue. The Yili Block …
Permian plume-strengthened Tarim lithosphere controls the Cenozoic deformation pattern of the Himalayan-Tibetan orogen
The high strength of the Tarim Basin (northwestern China) lithosphere, widely regarded as a
Precambrian craton, is evidenced by its resistance to Cenozoic deformation in the …
Precambrian craton, is evidenced by its resistance to Cenozoic deformation in the …
[HTML][HTML] Tracing the deep carbon cycle using metal stable isotopes: opportunities and challenges
The subduction of marine carbonates and carbonated oceanic crust to the Earth's interior
and the return of recycled carbon to the surface via volcanism may play a pivotal role in …
and the return of recycled carbon to the surface via volcanism may play a pivotal role in …
Using major element logratios to recognize compositional patterns of basalt: Implications for source lithological and compositional heterogeneities
ZF Yang, J Li, QB Jiang, F Xu, SY Guo… - … Research: Solid Earth, 2019 - Wiley Online Library
Understanding the source lithology of basalts can greatly impact our understanding of
magmatic processes, which can help us gain insight into mantle heterogeneity and crustal …
magmatic processes, which can help us gain insight into mantle heterogeneity and crustal …
Probing recycled carbonate in the lower mantle
Whether surficial carbonates can be carried into the Earth's lower mantle is key to global
deep carbon cycles but remains poorly understood. New clues from magnesium and zinc …
deep carbon cycles but remains poorly understood. New clues from magnesium and zinc …
Formation of Tarim large igneous province and strengthened lithosphere revealed through machine learning
Earth history is punctuated by voluminous magmatism and the formation of large igneous
provinces (LIPs). Although anomalous mantle temperatures are known to be involved in …
provinces (LIPs). Although anomalous mantle temperatures are known to be involved in …
Magnesium and calcium isotopic geochemistry of silica‐undersaturated alkaline basalts: Applications for tracing recycled carbon
Y Qi, Q Wang, GJ Wei, J Li… - Geochemistry …, 2022 - Wiley Online Library
Carbon plays important roles in the evolution of the atmosphere and biosphere, and
geochemical differentiation in Earth's interior. Most subducted C is recycled to the deep …
geochemical differentiation in Earth's interior. Most subducted C is recycled to the deep …
A mantle plume Connection for alkaline lamprophyres (Sannaites) from the Permian Tarim large igneous province: Petrological, geochemical and isotopic constraints
B Liu, Z Zhang, A Giuliani, Q Xie, W Kong… - Journal of …, 2023 - academic.oup.com
The origin of lamprophyres associated with large igneous provinces (LIPs) remains
controversial, particularly whether they are derived by direct melting of mantle plumes, or …
controversial, particularly whether they are derived by direct melting of mantle plumes, or …
Petrogenesis and tectonic significance of two bimodal volcanic stages from the Ediacaran Campo Alegre-Corupá Basin (Brazil): Record of metacratonization during …
Abstract The Ediacaran Campo Alegre-Corupá Basin in South Brazil developed in two
stages, the synorogenic passive rift (Basin Stage∼ 605–590 Ma) and the post-collisional …
stages, the synorogenic passive rift (Basin Stage∼ 605–590 Ma) and the post-collisional …