Zhiming Yang
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View article: Carbonate- and silicate-metasomatized mantle beneath Himalayan-Tibetan orogenic belt
Carbonate- and silicate-metasomatized mantle beneath Himalayan-Tibetan orogenic belt Open
View article: Spatiotemporal dependency data imputation for long-term health monitoring of concrete arch bridges
Spatiotemporal dependency data imputation for long-term health monitoring of concrete arch bridges Open
The structural health monitoring of bridge infrastructures is imperative for ensuring their uninterrupted functionality and mitigating potential hazards. Nevertheless, challenges arise Due to missing data and intricate latent dynamics embe…
View article: Redox state of subducted sediments controls porphyry copper mineralization along the Tethyan belt
Redox state of subducted sediments controls porphyry copper mineralization along the Tethyan belt Open
View article: Oxidized sediment recycling as a driver for postsubduction porphyry copper formation
Oxidized sediment recycling as a driver for postsubduction porphyry copper formation Open
The mechanisms driving the elevated oxidation state of postsubduction porphyry magmas and porphyry copper mineralization are still not fully understood. We present an integrated study of trace elemental and Mg-Hg isotopic compositions of p…
View article: Investigating the formation and enrichment processes of super-large North Sanshandao gold deposit (Jiaodong Peninsula, Eastern China): an in-depth mineralogical perspective
Investigating the formation and enrichment processes of super-large North Sanshandao gold deposit (Jiaodong Peninsula, Eastern China): an in-depth mineralogical perspective Open
The formation processes underlying super-large gold deposits present a captivating area of study, with a particularly enigmatic aspect being the mechanisms by which gold forms and accumulates within undersaturated hydrothermal fluids, nota…
View article: Carbonate- and silicate-metasomatized mantle beneath Himalayan-Tibetan orogenic belt
Carbonate- and silicate-metasomatized mantle beneath Himalayan-Tibetan orogenic belt Open
The extreme geochemical enrichment of post-collisional potassium-rich lava in the Alpine-Himalayan orogenic belt has led researchers to hypothesize that enrichment is inherited from a metasomatized mantle source potentially incorporating c…
View article: Copper and gold metallogeny in West China: An overview
Copper and gold metallogeny in West China: An overview Open
View article: Types of Subducted Material Controlling Tethyan Porphyry Copper Mineralization
Types of Subducted Material Controlling Tethyan Porphyry Copper Mineralization Open
The Tethyan orogenic belt underwent prolonged tectonic evolution and hosts numerous world-class porphyry copper deposits. Notably, most porphyry deposits are associated with Cenozoic continental collision, while fewer are formed during Mes…
View article: Quantitative Inversion of Martian Hydrous Minerals Based on LSTM-1DCNN Model
Quantitative Inversion of Martian Hydrous Minerals Based on LSTM-1DCNN Model Open
Hydrous minerals are significant indicators of the ancient aqueous environment on Mars, and orbital hyperspectral data are one of the most effective tools for obtaining information about the distribution of hydrous minerals on the Martian …
View article: Supplemental Material: Geology and genesis of the world-class wollastonite deposit at Shizhushan in South China and implications for exploration
Supplemental Material: Geology and genesis of the world-class wollastonite deposit at Shizhushan in South China and implications for exploration Open
Tables S1–S4 and Figure S1.
View article: Supplemental Material: Geology and genesis of the world-class wollastonite deposit at Shizhushan in South China and implications for exploration
Supplemental Material: Geology and genesis of the world-class wollastonite deposit at Shizhushan in South China and implications for exploration Open
Tables S1–S4 and Figure S1.
View article: Mercury isotope evidence for the importance of recycled fluids in collisional ore systems
Mercury isotope evidence for the importance of recycled fluids in collisional ore systems Open
The sources of fluids and metals in porphyry systems of continental-collision settings are poorly constrained. Mercury isotopes display unique mass-independent fractionation (expressed as Δ 199 Hg) and may provide important constraints on …
View article: Experimental evidence reveals the mobilization and mineralization processes of rare earth elements in carbonatites
Experimental evidence reveals the mobilization and mineralization processes of rare earth elements in carbonatites Open
Whereas the genesis of carbonatitic rare earth element (REE) deposits has long been a focus of study, the controls on mobilization and mineralization of REEs during magmatic-hydrothermal processes still remain open to debate. Here, we pres…
View article: Enrichment of Mississippi Valley-type (MVT) deposits in the Tethyan domain linked to organic matter-rich sediments
Enrichment of Mississippi Valley-type (MVT) deposits in the Tethyan domain linked to organic matter-rich sediments Open
View article: Trace-element analysis and radiometric dating by inductively coupled plasma–tandem mass spectrometry: Approaches and applications to metallogeny
Trace-element analysis and radiometric dating by inductively coupled plasma–tandem mass spectrometry: Approaches and applications to metallogeny Open
Inductively coupled plasma–tandem mass spectrometry (ICP–MS/MS) has rapidly established itself as a method for interference-free trace-element and isotope ratio analyses and has broad applications in geochemistry and geochronology, which a…
View article: Identification of recycled oceanic crust in the mantle source of sulfide-bearing lower crust of the Gangdese magmatic arc, Southern Tibet: Constraints from Sr–Nd–Li isotopes
Identification of recycled oceanic crust in the mantle source of sulfide-bearing lower crust of the Gangdese magmatic arc, Southern Tibet: Constraints from Sr–Nd–Li isotopes Open
Post-collisional porphyry copper deposit (PCD) is a new genetic type of PCDs discovered in the Himalayan–Tibetan orogenic belt. It is believed that the formation of ore-forming magmas results from the re-melting of a sulfide-bearing, thick…
View article: Gold remobilization of the Sanshandao gold deposit, Jiaodong Peninsula, Eastern China: Perspective from in-situ sulfide trace elements and sulfur isotopes
Gold remobilization of the Sanshandao gold deposit, Jiaodong Peninsula, Eastern China: Perspective from in-situ sulfide trace elements and sulfur isotopes Open
The Sanshandao is a typical altered-rock-style gold deposit (>260 t @ 3.96 g/t). The deposit is located at the northernmost end of the NE-trending Sanshandao fault in the northwestern Jiaodong Peninsula. The orebodies are mainly hosted by …
View article: Metallogeny of the Xiaotongjiapuzi gold deposit, Liaodong Peninsula (Eastern China): Perspective from sulfide trace element geochemistry and sulfur isotopes
Metallogeny of the Xiaotongjiapuzi gold deposit, Liaodong Peninsula (Eastern China): Perspective from sulfide trace element geochemistry and sulfur isotopes Open
Most gold ores have variable sulfur isotopic and trace elemental compositions at micro-/nano-scale, which makes the understanding of the gold formation process more challenging. The advancement of in-situ analytical techniques offer opport…
View article: Long-lived magmatic evolution and mineralization resulted in formation of the giant Cuonadong Sn-W-Be polymetallic deposit, southern Tibet
Long-lived magmatic evolution and mineralization resulted in formation of the giant Cuonadong Sn-W-Be polymetallic deposit, southern Tibet Open
The Cuonadong Sn-W-Be polymetallic deposit is the first Cenozoic leucogranite-related rare-metal deposit with giant metallogenic potential in the Himalayan orogen. However, the controlling factors for the supernormal enrichment of berylliu…
View article: Generation of the Early Cretaceous granitoid in the Dazeshan region, Jiaodong Peninsula: Implications for the crustal reworking in the North China Craton
Generation of the Early Cretaceous granitoid in the Dazeshan region, Jiaodong Peninsula: Implications for the crustal reworking in the North China Craton Open
Lower crust-derived granitic rocks provide constraints on the crustal reworking process and consequently give hints on the destruction mechanism of the cratons. The North China Craton (NCC) underwent extensive crustal melting in the Mesozo…
View article: Petrogenesis of Mesozoic Magmatic Suites in the Jiaodong Peninsula: Implications for Crust-Mantle Interactions and Decratonization
Petrogenesis of Mesozoic Magmatic Suites in the Jiaodong Peninsula: Implications for Crust-Mantle Interactions and Decratonization Open
The North China Craton (NCC) has thick lithosphere in the Paleozoic (>200 km) but appears to be decratonized in the Mesozoic. However, the actual processes operated in the lower crust-deep mantle are still unclear. The Mesozoic granitic…
View article: Partial melting of amphibolitic lower crust and subsequent melt-crystal separation for generation of the Early Eocene magmatism in eastern Himalaya
Partial melting of amphibolitic lower crust and subsequent melt-crystal separation for generation of the Early Eocene magmatism in eastern Himalaya Open
The Himalayan leucogranites provide a good opportunity to investigate the crustal evolution of the southern Qinghai-Tibet Plateau. In this study, we present zircon U-Pb and monazite U-Th-Pb ages, zircon Hf isotopes and whole-rock Sr-Nd-Pb …
View article: Incident Risk and Burden of Cardiovascular Diseases Attributable to Long-Term NO2 Exposure in Chinese Adults
Incident Risk and Burden of Cardiovascular Diseases Attributable to Long-Term NO2 Exposure in Chinese Adults Open
View article: Possible source of Au in the Jiaodong area from lower crustal sulfide cumulates: Evidence from oxygen states and chalcophile elements contents of Mesozoic magmatic suites
Possible source of Au in the Jiaodong area from lower crustal sulfide cumulates: Evidence from oxygen states and chalcophile elements contents of Mesozoic magmatic suites Open
The genesis of giant Jiaodong gold province remains perplexing although many ore-forming models have been proposed in the past decades. The key issues are what caused the burst of gold around 120 Ma and possible sources of gold. Here we re…
View article: Latest Oligocene adakitic rocks in western Iran: implications for early crustal thickening and tectonic evolution of Iran Block
Latest Oligocene adakitic rocks in western Iran: implications for early crustal thickening and tectonic evolution of Iran Block Open
Supplementary Table 2
View article: Sex Disparity in Cognitive Aging Related to Later-Life Exposure To Ambient Air Pollution
Sex Disparity in Cognitive Aging Related to Later-Life Exposure To Ambient Air Pollution Open
View article: Source and evolution of the ore-forming fluid of the Cuonadong Sn-W-Be polymetallic deposit (southern Tibet, China): Constraints from scheelite trace element and Sr isotope geochemistry
Source and evolution of the ore-forming fluid of the Cuonadong Sn-W-Be polymetallic deposit (southern Tibet, China): Constraints from scheelite trace element and Sr isotope geochemistry Open
The Cuonadong Sn-W-Be polymetallic deposit is the first rare-metal deposit with an extraordinary metallogenic potential that has been discovered in the Tethyan Himalayan metallogenic belt. The deposit shows a wide range of different minera…
View article: Mineral Resource Science in China: Review and perspective
Mineral Resource Science in China: Review and perspective Open
Mineral resources are essential to prosperity and security of modern societies. How mineral resources can guarantee sustainable development of economy in countries, especially those developing countries, has long been a focus of attention …
View article: Contrasting Porphyry Cu Fertilities in the Yidun Arc, Eastern Tibet: Insights from Zircon and Apatite Compositions and Implications for Exploration
Contrasting Porphyry Cu Fertilities in the Yidun Arc, Eastern Tibet: Insights from Zircon and Apatite Compositions and Implications for Exploration Open
The Yidun arc, part of the Sanjiang Paleo-Tethyan orogenic belt in eastern Tibet, hosts several porphyry Cu deposits in its southern section, whereas abundant contemporaneous but barren granitoid intrusions occur in the northern section. H…
View article: Supplemental Material: Redox state of southern Tibetan upper mantle and ultrapotassic magmas
Supplemental Material: Redox state of southern Tibetan upper mantle and ultrapotassic magmas Open
Methods, Tables S1–S7, and Figures S1–S8