Mei‐Fu Zhou
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View article: Subsoiling-Induced Shifts in Nitrogen Dynamics and Microbial Community Structure in Semi-Arid Rainfed Maize Agroecosystems
Subsoiling-Induced Shifts in Nitrogen Dynamics and Microbial Community Structure in Semi-Arid Rainfed Maize Agroecosystems Open
Global agricultural intensification has exacerbated soil compaction and nitrogen (N) inefficiency, thereby threatening sustainable crop production. Sub-soiling, a tillage technique that fractures subsurface layers while preserving surface …
View article: Effects of Subsolidus Cooling on the Redox State of the Oceanic Upper Mantle
Effects of Subsolidus Cooling on the Redox State of the Oceanic Upper Mantle Open
Oxygen fugacity (fO2) of the oceanic upper mantle is commonly determined using the olivine–orthopyroxene–spinel (ol–opx–sp) oxybarometer based on Fe2+/Fe3+ equilibrium among these minerals. However, rapid Fe redistribution during subsolidu…
View article: Terrestrial temperature history reveals Late Miocene rapid uplift of the northern Tibetan Plateau
Terrestrial temperature history reveals Late Miocene rapid uplift of the northern Tibetan Plateau Open
Paleoaltimetry data are essential for deciphering the growth trajectory of orogenic plateaus and underlying forcing mechanisms. However, paleoaltitude reconstructions using conventional paleotemperature analysis often have low resolution o…
View article: Heavy boron isotopes in intraplate basalts reveal recycled carbonate in the mantle
Heavy boron isotopes in intraplate basalts reveal recycled carbonate in the mantle Open
Recycling of surficial volatiles such as carbon into the mantle plays a fundamental role in modulating Earth’s habitability. However, slab devolatilization during subduction could prevent carbon from entering the deep mantle. Boron isotope…
View article: Whole-rock and mineral compositions of harzburgites in the Luobusa ophiolite, Tibet
Whole-rock and mineral compositions of harzburgites in the Luobusa ophiolite, Tibet Open
Whole-rock and mineral compositions of harzburgites in the Luobusa ophiolite, Tibet
View article: Publisher Correction: Diversities of chromite mineralization induced by chemo–thermal evolution of the mantle during subduction initiation
Publisher Correction: Diversities of chromite mineralization induced by chemo–thermal evolution of the mantle during subduction initiation Open
View article: Diversities of chromite mineralization induced by chemo–thermal evolution of the mantle during subduction initiation
Diversities of chromite mineralization induced by chemo–thermal evolution of the mantle during subduction initiation Open
Ophiolites, mostly formed via subduction initiation at proto-forearcs, exhibit a unique variation of mantle-derived magmatism from MORB-like to low-Ti tholeiitic and bainitic-like affinities. Such variation was suggested to form chromite d…
View article: Cassiterite and zircon U-Pb ages and compositions from ore-bearing and barren granites in Thailand: Constraints on the formation of tin deposits in Southeast Asia
Cassiterite and zircon U-Pb ages and compositions from ore-bearing and barren granites in Thailand: Constraints on the formation of tin deposits in Southeast Asia Open
View article: Characterization of regolith-hosted rare earth element deposits using reflectance spectroscopy: Framework towards an efficient and reliable field exploration tool
Characterization of regolith-hosted rare earth element deposits using reflectance spectroscopy: Framework towards an efficient and reliable field exploration tool Open
View article: Hyper-enrichment of heavy rare earth elements in highly evolved granites through multiple hydrothermal mobilizations
Hyper-enrichment of heavy rare earth elements in highly evolved granites through multiple hydrothermal mobilizations Open
Highly evolved granites can be important hosts of rare earth element (REE) resources, and more importantly, they commonly serve as the protolith for regolith-hosted REE deposits to form during weathering. Highly evolved granites in the Zud…
View article: Deposit type discrimination based on trace elements in sphalerite
Deposit type discrimination based on trace elements in sphalerite Open
Sphalerite can form in different geological environments and is the main ore mineral of most Pb-Zn deposits. Trace elements in sphalerite combined with machine learning (ML) methods have been used for deposit type discrimination. However, …
View article: In-Situ Element and U-Pb Age of Cassiterite from the Gejiu and Dulong Tin Deposits in Southwestern China: New Constraints on Ore Genesis and Their Linkage to the Se Asia Tin Belt
In-Situ Element and U-Pb Age of Cassiterite from the Gejiu and Dulong Tin Deposits in Southwestern China: New Constraints on Ore Genesis and Their Linkage to the Se Asia Tin Belt Open
View article: Germanium-rich nanoparticles in Cu-poor sphalerite: A new mechanism for Ge enrichment
Germanium-rich nanoparticles in Cu-poor sphalerite: A new mechanism for Ge enrichment Open
Germanium (Ge) is a critical raw material used in high-technology industry (i.e., optical industry) applications, and it is predominantly concentrated in coals and Zn-rich deposits. Previous studies on Zn-rich deposits have documented a co…
View article: Constraints of in-situ S-isotopic compositions of pyrite on the genesis of the Bayinqinggeli sandstone-hosted uranium deposit, Ordos Basin, Northern China
Constraints of in-situ S-isotopic compositions of pyrite on the genesis of the Bayinqinggeli sandstone-hosted uranium deposit, Ordos Basin, Northern China Open
Sandstone-hosted uranium deposits are formed by redox interactions between oxidized ore-forming fluids and sufficient reductants, such as sulfide and organic materials within hosting strata, or hydrocarbon-bearing fluids from deep reservoi…
View article: A Paleozoic mercury mineralisation event in South China: In situ U-Pb dating and chemical compositions of calcite from the Jianyan Hg deposit
A Paleozoic mercury mineralisation event in South China: In situ U-Pb dating and chemical compositions of calcite from the Jianyan Hg deposit Open
View article: Evolution of pegmatite recorded by zoned garnet from the No. 9 dike in the Jiajika Li polymetallic deposit, eastern Tibetan plateau
Evolution of pegmatite recorded by zoned garnet from the No. 9 dike in the Jiajika Li polymetallic deposit, eastern Tibetan plateau Open
Granitic pegmatites can be extremely rich in Li, an important metal for modern industries. Being the Asia's largest hard-rock Li polymetallic deposit, the Jiajika Li deposit is associated with numerous pegmatite dikes in the eastern Tibeta…
View article: An Unusually Warm Upper‐Crust in the Late Paleozoic North China Continental Arc: Implications for the Thermal Modification of the Giant Bayan Obo REE Deposit
An Unusually Warm Upper‐Crust in the Late Paleozoic North China Continental Arc: Implications for the Thermal Modification of the Giant Bayan Obo REE Deposit Open
The genesis and timing of formation of the giant Bayan Obo deposit, the world's largest rare earth element (REE) deposit in the western part of the late Paleozoic northern North China continental arc (NCA), are highly controversial due to …
View article: Ground ice-magma interaction resurfaced the landing region of the Zhurong rover during the Amazonian
Ground ice-magma interaction resurfaced the landing region of the Zhurong rover during the Amazonian Open
Despite a consensus view that Mars has been cold and icy throughout the Amazonian (3 billion years ago until present), the Zhurong rover has provided striking evidence for aqueous resurfacing processes in and around the landing site during…
View article: Lithium Isotope Fractionation During Intensive Felsic Magmatic Differentiation
Lithium Isotope Fractionation During Intensive Felsic Magmatic Differentiation Open
The Xihuashan and Yaogangxian granitic plutons in South China comprise highly evolved multiphase Li‐rich granites and host quartz‐vein‐type tungsten deposits. The δ 7 Li values of Phase A (early stage), B (middle stage), and C (late stage)…
View article: Supplementary Tables for 'Trans-Lithospheric Ascent Processes of the Deep-Rooted Magma Plumbing System underneath the Ultraslow-Spreading SW Indian Ridge'
Supplementary Tables for 'Trans-Lithospheric Ascent Processes of the Deep-Rooted Magma Plumbing System underneath the Ultraslow-Spreading SW Indian Ridge' Open
Supplementary Tables
View article: Compositions of minerals from the Coto high-Al chromite deposit, Zambales ophiolite, Philippines
Compositions of minerals from the Coto high-Al chromite deposit, Zambales ophiolite, Philippines Open
This dataset presents a series of elemental and isotopic compositions for rocks collected from the Coto high-Al chromite deposit, Zambales ophiolite, Philippines, including the major element compositions of chromite and in-situ Li isotopic…
View article: Supplementary Tables for 'Trans-Lithospheric Ascent Processes of the Deep-Rooted Magma Plumbing System underneath the Ultraslow-Spreading SW Indian Ridge'
Supplementary Tables for 'Trans-Lithospheric Ascent Processes of the Deep-Rooted Magma Plumbing System underneath the Ultraslow-Spreading SW Indian Ridge' Open
Supplementary Tables
View article: Lithium Isotope Fractionation during Intensive Felsic Magmatic Differentiation
Lithium Isotope Fractionation during Intensive Felsic Magmatic Differentiation Open
All the isotope and element data of the manuscript "Lithium isotope fractionation during intensive felsic magmatic differentiation". Table 1 Major elemental compositions (in wt.%) for granites from the Xihuashan and Yaogangxian plutons
View article: Lithium Isotope Fractionation during Intensive Felsic Magmatic Differentiation
Lithium Isotope Fractionation during Intensive Felsic Magmatic Differentiation Open
All the isotope and element data of the manuscript "Lithium isotope fractionation during intensive felsic magmatic differentiation". Table 1 Major elemental compositions (in wt.%) for granites from the Xihuashan and Yaogangxian plutons
View article: Microorganisms Accelerate REE Mineralization in Supergene Environments
Microorganisms Accelerate REE Mineralization in Supergene Environments Open
Understanding the role of microorganisms in the formation of regolith-hosted rare earth element (REE) deposits is beneficial for improving the metallogenic theory and deposit exploitation, given that such deposits absolutely exist in subtr…
View article: Germanium enrichment in sphalerite with acicular and euhedral textures: an example from the Zhulingou carbonate-hosted Zn(-Ge) deposit, South China
Germanium enrichment in sphalerite with acicular and euhedral textures: an example from the Zhulingou carbonate-hosted Zn(-Ge) deposit, South China Open
View article: Kinetic controls on Sc distribution in diopside and geochemical behavior of Sc in magmatic systems
Kinetic controls on Sc distribution in diopside and geochemical behavior of Sc in magmatic systems Open
View article: Growth and thermal maturation of the Toba magma reservoir
Growth and thermal maturation of the Toba magma reservoir Open
View article: Growth and thermal maturation of the Toba magma reservoir
Growth and thermal maturation of the Toba magma reservoir Open
Significance Understanding the thermal state of magma reservoirs before supereruptions is crucial for interpreting the processes leading to such catastrophic events. Here, we show that the two supereruptions of Toba were preceded and follo…
View article: Intense subaerial weathering of eolian sediments in Gale crater, Mars
Intense subaerial weathering of eolian sediments in Gale crater, Mars Open
Clay-bearing sedimentary rocks at Gale crater are more consistent with subaerial chemical weathering than formation in a lake.