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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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Bohaiwan Basin (4)
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Da Hinggan Ling (1)
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Guangxi China (1)
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Japan
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Pacific Ocean
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Yellow Sea
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elements, isotopes
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stable isotopes
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Lu/Hf (1)
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metals
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iron
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rare earths
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samarium
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noble gases
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oxygen
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selenium (1)
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sulfur
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fossils
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Chordata
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Eutheria
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Carnivora
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Invertebrata
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sulfates
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Primary terms
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Asia
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Far East
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China
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Bohaiwan Basin (4)
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Da Hinggan Ling (1)
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Guangxi China (1)
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Hebei China (6)
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Heilongjiang China (1)
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Inner Mongolia China (3)
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North China Platform (7)
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Xinjiang China
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Japan
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Kyushu (1)
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Taiwan (1)
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biogeography (1)
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bitumens (2)
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carbon
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C-13/C-12 (1)
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Cenozoic
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Quaternary
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Pleistocene (1)
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Tertiary
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Neogene
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Miocene
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Guantao Formation (1)
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Paleogene
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Dongying Formation (1)
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Eocene (1)
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Shahejie Formation (4)
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Chordata
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Vertebrata
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Tetrapoda
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Mammalia
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Theria
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Eutheria
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Carnivora
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Qinhuangdao China
Sedimentary characteristics and genetic mechanisms of high-quality reservoirs in a mixed siliciclastic-carbonate system in the Qinhuangdao area, Bohai Sea, China
Location of the study area of the Qinhuangdao area of the Bohai Sea, China....
Where and when the Palaeo-Asian Ocean was closed: new evidence from the Tuquan ophiolite
Microstructural observations of clay-hosted pores in black shales: implications for porosity preservation and petrophysical variability
Effects of the coupling between slope morphology and bottom currents on flow erosion and sedimentation at the Dongsha Continental Margin, South China Sea
Geology and Geochemistry of the Jianshan Banded Iron Formation in Shanxi Province, China: Constraints on the Genesis
Petrogenesis and tectonic setting of the Huhetaoergai granitic pluton in the northern Ya-Gan Fault zone, northern Alxa, China: constraints from whole-rock geochemistry, zircon U–Pb ages, and Hf isotope compositions
Origin of Late Palaeozoic bauxites in the North China Craton: constraints from zircon U–Pb geochronology and in situ Hf isotopes
The Hadamengou K-feldspar–quartz vein-type Au mineralization in the northern margin of the North China Craton (China): an Indosinian oxidized intrusion-related Au–(Mo) system?
Geology and geochemistry of the Yuanjiacun banded iron formation in Shanxi Province, China: constraints on the genesis
Natural evidence of organic nanostructure transformation of shale during bedding-parallel slip
The mechanism behind pressure-induced isosymmetric second-order phase transitions
A review of the genesis, evolution, and prediction of natural fractures in deep tight sandstones of China
Magnetic collapse and low conductivity of Fe 3 N in the deep interiors of Earth-like planets
Equation of state and structural evolution of manganese dolomite (kutnohorite) under high pressures
Seismic interpretation of sandstone-type uranium deposits in the Songliao Basin, Northeast China
Circa 2.5 Ga granitoids in the eastern North China craton: Melting from ca. 2.7 Ga accretionary crust
Abstract Characterization of the evolution of delta lobes has theoretical significance for the formation of entire deltas. The Diaokou lobe of the Yellow River delta provides a typical example. The Yellow River transported a great deal of sediment to the Diaokou area during the period of 1964–76 after the river changed its course to the Diaokou River and formed a new delta lobe – the Diaokou lobe. The Diaokou lobe reflects the evolution of the modern Yellow River delta and contains a record that represents the complete modern Yellow River delta depositional system. Using grain-size characteristics, magnetism, and the accelerator mass spectrometry (AMS) 14 C dating of cores ZK10-3 and ZK30 in the northern part of the Diaokou lobe, combined with collected data from cores ZK227, ZK1 and ZK228, which are located further south on the Diaokou lobe, we analysed the Holocene and recent stratigraphy of the Diaokou lobe area and its evolution. The Holocene stratigraphy of the Diaokou lobe and the nearby area contains upwards-succession, shallow-marine, river and lake, salt-marsh, and delta facies. This area received deltaic deposits beginning in 1855 and experienced prodelta, delta-front (lateral) and delta-plain deposition. When the Diaokou lobe began to form, this area experienced four stages of deposition after 1964: (1) dispersed-flow deposition; (2) single-channel deposition; (3) diversion deposition; and (4) abandonment and erosion. Compared with the evolution of a lobe of the Mississippi delta, the Yellow River delta contains thick, laterally extensive deposits as a result of the higher sediment load.