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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Far East
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China
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Da Hinggan Ling (29)
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Heilongjiang China (5)
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Inner Mongolia China (10)
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Jilin China (1)
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North China Plain (1)
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Songliao Basin (1)
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Mongolia (1)
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Siberia (1)
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Transbaikalia (1)
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Zabaykalskiy Russian Federation (1)
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Commonwealth of Independent States
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Russian Federation
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Eurasia (1)
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commodities
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brines (1)
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metal ores
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base metals (1)
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copper ores (3)
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gold ores (3)
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iron ores (1)
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lead ores (9)
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lead-zinc deposits (8)
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molybdenum ores (4)
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polymetallic ores (4)
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silver ores (6)
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tin ores (3)
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zinc ores (10)
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mineral deposits, genesis (9)
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elements, isotopes
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hydrogen
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D/H (1)
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isotope ratios (16)
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isotopes
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (4)
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Pb-208/Pb-204 (4)
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stable isotopes
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D/H (1)
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Hf-177/Hf-176 (5)
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Nd-144/Nd-143 (3)
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O-18/O-16 (3)
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (4)
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Pb-208/Pb-204 (4)
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S-34/S-32 (4)
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Sr-87/Sr-86 (4)
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large-ion lithophile elements (1)
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Lu/Hf (1)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (4)
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gold (1)
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hafnium
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Hf-177/Hf-176 (5)
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lead
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (4)
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Pb-208/Pb-204 (4)
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rare earths
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tin (1)
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oxygen
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selenium (2)
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sulfur
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geochronology methods
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Ar/Ar (2)
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U/Pb (15)
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geologic age
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Cenozoic
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metamorphic rocks
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sheet silicates
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illite (1)
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tellurides
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Primary terms
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absolute age (16)
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Asia
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Far East
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China
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Da Hinggan Ling (29)
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Heilongjiang China (5)
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Inner Mongolia China (10)
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Jilin China (1)
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North China Plain (1)
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Songliao Basin (1)
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Mongolia (1)
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Siberia (1)
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Transbaikalia (1)
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Zabaykalskiy Russian Federation (1)
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brines (1)
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Cenozoic
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Tertiary
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crust (5)
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hydrogen
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igneous rocks
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plutonic rocks
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diabase (1)
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diorites (3)
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gabbros (3)
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granites
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A-type granites (1)
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granite porphyry (4)
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I-type granites (2)
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monzogranite (2)
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granodiorites (3)
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monzodiorite (1)
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syenites (1)
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volcanic rocks
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andesites (1)
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basalts (1)
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dacites (1)
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rhyolites (3)
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trachyandesites (1)
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inclusions
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fluid inclusions (5)
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intrusions (8)
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isotopes
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radioactive isotopes
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (4)
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Pb-208/Pb-204 (4)
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stable isotopes
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D/H (1)
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Hf-177/Hf-176 (5)
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Nd-144/Nd-143 (3)
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O-18/O-16 (3)
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (4)
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Pb-208/Pb-204 (4)
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S-34/S-32 (4)
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Sr-87/Sr-86 (4)
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magmas (4)
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mantle (5)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Berriasian (1)
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Hauterivian (1)
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Valanginian (1)
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Upper Cretaceous (1)
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Jurassic
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Upper Jurassic
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Tithonian (1)
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Triassic
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Lower Triassic (2)
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upper Mesozoic (1)
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metal ores
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base metals (1)
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copper ores (3)
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gold ores (3)
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iron ores (1)
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lead ores (9)
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lead-zinc deposits (8)
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molybdenum ores (4)
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polymetallic ores (4)
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silver ores (6)
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tin ores (3)
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tungsten ores (1)
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zinc ores (10)
-
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (4)
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gold (1)
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hafnium
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Hf-177/Hf-176 (5)
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lead
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Pb-206/Pb-204 (3)
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Pb-207/Pb-204 (4)
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Pb-208/Pb-204 (4)
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rare earths
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neodymium
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Nd-144/Nd-143 (3)
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tin (1)
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tungsten (1)
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metamorphic rocks
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metasomatic rocks
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skarn (4)
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metasomatism (3)
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mineral deposits, genesis (9)
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mineral exploration (3)
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oxygen
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O-18/O-16 (3)
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Paleozoic
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Cambrian
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Upper Cambrian (1)
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Ordovician
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Permian
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Lower Permian (2)
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paragenesis (3)
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roads (1)
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selenium (2)
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slope stability (1)
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soil mechanics (1)
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sulfur
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tectonics (6)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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sandstone (1)
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shale (1)
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siltstone (1)
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Da Hinggan Ling
Controls on the formation of porphyry Mo deposits: Insights from porphyry (-skarn) Mo deposits in northeastern China
Fluid evolution and ore genesis of Cu–Pb–Zn veins in the Panjiaduan deposit, Great Xing’an Range, NE China: evidence from fluid inclusion and H–O–He–Ar isotopes
Study on Stability Analysis of Soil-Rock-Mixture Slopes under Freeze-Thaw Erosion in Greater Khingan Mountains
Geochronology, geochemistry, and petrogenesis of Early Cretaceous highly differentiated I-type granites in the central Great Xing’an Range, northeastern China
Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing’an Range W belt, NE China: insights from the Narenwula Complex
Abstract The Halaha River–Chaoer River (HC) volcanic field in the Greater Hinggan Mountain Range (NE China) consists of at least 41 monogenetic basaltic volcanoes. Strombolian, violent Strombolian and phreatomagmatic eruptions, as well as the transitional eruptions, generated simple volcanic cones (single vent) and composite volcanic cones (multiple vents). The simple elongated cone is the most abundant geomorphology type. By analysing the elongated crater and coalescent aligned circular crater, cone breaching and depression, and aligned vents, we identified a number of magma-feeding fissures. The majority of these fissures strike NE–ENE. Accordingly, we infer that the regional stress field affected volcanism in the HC field. The lavas in this field are alkali basalts that are enriched in light rare earth elements (La/Yb N = 7.9–24.5). Their ocean island basalt-like rare earth element and spider-diagram patterns, high Nb/U ratios and high TiO 2 contents (>2 wt%) indicate that the basalts were derived from the asthenosphere mantle. Both the asthenosphere upwelling and the tectonic forces are the key controlling factors of the volcanism in the HC field.