What is he best known for?
The fields of study he is best known for:
- Basalt
- Mineral
- Igneous rock
The scientist’s investigation covers issues in Geochemistry, Basalt, Flood basalt, Olivine and Large igneous province.
His Geochemistry study integrates concerns from other disciplines, such as Sulfide and Mineralogy.
The various areas that Liang Qi examines in his Olivine study include Chromite and Mantle.
The study incorporates disciplines such as Picrite basalt, Ultramafic rock and Oceanic crust in addition to Mantle.
His work focuses on many connections between Large igneous province and other disciplines, such as Layered intrusion, that overlap with his field of interest in Diorite.
In his work, Analytical chemistry and Inductively coupled plasma mass spectrometry is strongly intertwined with Metallurgy, which is a subfield of Platinum group.
His most cited work include:
- Subduction-related origin of the 750 Ma Xuelongbao adakitic complex (Sichuan Province, China): Implications for the tectonic setting of the giant Neoproterozoic magmatic event in South China (230 citations)
- REE and PGE Geochemical Constraints on the Formation of Dunites in the Luobusa Ophiolite, Southern Tibet (219 citations)
- Permian flood basalts and mafic intrusions in the Jinping (SW China)–Song Da (northern Vietnam) district: Mantle sources, crustal contamination and sulfide segregation (168 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Geochemistry, Basalt, Mineralogy, Mantle and Platinum group.
Liang Qi has included themes like Sulfide and Large igneous province in his Geochemistry study.
The concepts of his Mineralogy study are interwoven with issues in Magnetite, Trace element, Mineralization and Nuclear chemistry.
In his research on the topic of Mantle, Forearc and Peridotite is strongly related with Ophiolite.
His study looks at the relationship between Platinum group and topics such as Metallurgy, which overlap with Certified reference materials and Analytical chemistry.
His research in Olivine intersects with topics in Chromite and Ultramafic rock.
He most often published in these fields:
- Geochemistry (90.40%)
- Basalt (32.00%)
- Mineralogy (28.00%)
What were the highlights of his more recent work (between 2015-2021)?
- Geochemistry (90.40%)
- Molybdenite (12.00%)
- Pyrite (11.20%)
In recent papers he was focusing on the following fields of study:
Liang Qi mainly investigates Geochemistry, Molybdenite, Pyrite, Trace element and Isochron.
His Geochemistry research incorporates themes from Skarn and Mineralization.
His Molybdenite research incorporates elements of Radiochemistry, Inductively coupled plasma mass spectrometry, Rhenium and Aqua regia.
His Trace element course of study focuses on Mineralogy and Carbonate, Digestion, Relative standard deviation and Bauxite.
His Isochron research includes themes of Hydrothermal circulation, Mafic and Proterozoic.
His biological study spans a wide range of topics, including Subduction and Basalt.
Between 2015 and 2021, his most popular works were:
- Geochronological, Petrological, and Geochemical Constraints on Ni-Cu Sulfide Mineralization in the Poyi Ultramafic-Troctolitic Intrusion in the Northeast Rim of the Tarim Craton, Western China (41 citations)
- Origin of the volcanic-hosted Yamansu Fe deposit, Eastern Tianshan, NW China: constraints from pyrite Re-Os isotopes, stable isotopes, and in situ magnetite trace elements (25 citations)
- In-situ LA–ICP–MS trace elements analysis of magnetite: The Fenghuangshan Cu–Fe–Au deposit, Tongling, Eastern China (25 citations)
In his most recent research, the most cited papers focused on:
- Mineral
- Basalt
- Igneous rock
Geochemistry, Skarn, Calcite, Magnetite and Trace element are his primary areas of study.
The Geochemistry study combines topics in areas such as Sulfide, Mineralization and Meteoric water.
Liang Qi focuses mostly in the field of Sulfide, narrowing it down to topics relating to Mantle and, in certain cases, Dike.
His Mineralization research is multidisciplinary, incorporating perspectives in Carbonate, Chalcopyrite and Mineralogy.
His work carried out in the field of Meteoric water brings together such families of science as Isochron and Pyrite.
His Olivine research extends to Zircon, which is thematically connected.
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