Refine
Year of publication
Document Type
- Article (147)
- Preprint (93)
- Working Paper (1)
Language
- English (241)
Has Fulltext
- yes (241)
Is part of the Bibliography
- no (241)
Keywords
- BESIII (14)
- Branching fraction (9)
- e +-e − Experiments (9)
- Hadronic decays (5)
- Particle and Resonance Production (5)
- Quarkonium (5)
- Branching fractions (4)
- Lepton colliders (4)
- Charm Physics (3)
- Charmed mesons (3)
- Charmonium (3)
- Electroweak interaction (3)
- Exotics (3)
- Initial state radiation (3)
- Polarization (3)
- Spectroscopy (3)
- e+-e− Experiments (3)
- Bhabha (2)
- Charm physics (2)
- Collectivity (2)
- Correlation (2)
- Cross section (2)
- Elastic scattering (2)
- Electroweak Interaction (2)
- Hadronic cross section (2)
- Leptonic, semileptonic & radiative decays (2)
- Muon anomaly (2)
- Particle decays (2)
- Pion form factor (2)
- QCD (2)
- RHIC (2)
- Shear viscosity (2)
- minerals (2)
- Angular distribution (1)
- Annihilation (1)
- BESIII detector (1)
- Born cross section measurement (1)
- CP violation (1)
- Charged-particle multiplicity (1)
- Charmonia (1)
- Charmonium (-like) (1)
- Cold nuclear matter effects (1)
- Covariance matrix (1)
- Cross section measurements (1)
- D meson (1)
- D0 and D+ mesons (1)
- Dalitz decay (1)
- Dark photon (1)
- Dark sector (1)
- Datong coalfield (1)
- Di-hadron correlations (1)
- Diffraction (1)
- D⁰ meson (1)
- Early Permian (1)
- Electromagnetic form factor (1)
- Electromagnetic form factors (1)
- Experimental nuclear physics (1)
- Experimental particle physics (1)
- FOS: Physical sciences (1)
- Flavor changing neutral currents (1)
- Flavor symmetries (1)
- Flavour Physics (1)
- Flow (1)
- Form factors (1)
- Groomed jet radius (1)
- Hadronization (1)
- Hadrons (1)
- Heavy ion collisions (1)
- Heavy-ion (1)
- High Energy Physics - Experiment (hep-ex) (1)
- Hyperons (1)
- Interference fragmentation function (1)
- Invisible decays (1)
- J/ψ suppression (1)
- Jet substructure (1)
- Multiple parton interactions (1)
- Net-charge correlations (1)
- Net-charge fluctuations (1)
- Neutrinos (1)
- Nonflow (1)
- Particle and resonance production (1)
- Particle phenomena (1)
- Proton (1)
- Proton-proton collisions (1)
- Quantum chromodynamics (1)
- R value (1)
- Radiative decay (1)
- Rare decays (1)
- STAR (1)
- Semi-leptonic decays (1)
- SoftDrop (1)
- Spin alignment (1)
- Splitting function (1)
- Techniques Electromagnetic calorimeters (1)
- Transversity (1)
- Triple quarkonia (1)
- Y (4260) (1)
- Y states (1)
- center-of-mass energy (1)
- charmonium-like states (1)
- coal (1)
- dimuon (1)
- diphoton (1)
- e+e − annihilation (1)
- e+e⁻ − Experiments (1)
- e+e− Experiments (1)
- e+e− annihilation (1)
- ectosomes (1)
- electron-positron collision (1)
- exosomes (1)
- extracellular vesicles (1)
- felsic detrital (1)
- guidelines (1)
- hadron spectroscopy (1)
- hadronic events (1)
- helicity amplitude analysis (1)
- hydrothermal fluids (1)
- inclusive J/ψ decays (1)
- lithium (1)
- luminosity (1)
- microparticles (1)
- microvesicles (1)
- minimal information requirements (1)
- number of J/ψ events (1)
- p+p collisions (1)
- reproducibility (1)
- rigor (1)
- seawater influence (1)
- standardization (1)
- terrigenous (1)
- tetraquark (1)
- trace elements (1)
- trigger efficiency (1)
- Λ+c baryon (1)
- Σ hyperon (1)
The Early Permian coal is of great value in the Tengxian Coalfield, Shandon Province, Eastern China. This work deals with the new data focusing on mineralogical characteristics in the Early Permian Shanxi Formation No. 3 coal from the Jinyuan Mine. The Jinyuan coal is a low ash and highly volatile A bituminous coal. Minerals in the No. 3 coal mainly comprise of kaolinite, ankerite, illite, calcite, siderite, and quartz, with varying compositions of trace amounts of pyrite, jarosite, bassanite, anatase, and rutile. According to mineral assemblage in the coal plies, three Types (A to C) can be identified in the No. 3 coal. The dominant minerals in Type A are poorly-ordered kaolinite, illite, quartz, pyrite, and jarosite. Type B is mainly composed of well-ordered kaolinite, illite, siderite, ankerite, and calcite. Type C, with just one sample (JY-3-7c), which contains high proportions of calcite (54%) and ankerite (34%). Terrigenous minerals are elevated in coal plies that typically have relatively high contents of ash yield. The formation of syngenetic pyrite was generally due to seawater, while the sulphate minerals (jarosite and coquimbite) were derived from the oxidation of pyrite. Epigenetic vein-like or fracture-fillings carbonate minerals (ankerite, calcite, and siderite), kaolinite, and pyrite, as well as authigenic quartz were derived from the influx of hydrothermal fluids during different periods, from the authigenic to epigenetic. The paragonite in the coal may have been formed by the precipitated from Na-rich hydrothermal fluids. No effects of magmatic intrusion on mineralogy were investigated in this research.