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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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Altai Mountains
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Gorny Altai (1)
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Kuznetsk Alatau (1)
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Altai Russian Federation
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Gorny Altai (1)
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Altai-Sayan region (1)
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Far East
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China
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Sichuan China (1)
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Yangtze Platform (1)
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Salair Ridge (1)
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West Siberia
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Kuznetsk Alatau (1)
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Caledonides (1)
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Commonwealth of Independent States
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Russian Federation
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Altai Russian Federation
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Gorny Altai (1)
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Kuznetsk Alatau (1)
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Salair Ridge (1)
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West Siberia
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Kuznetsk Alatau (1)
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Europe
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Variscides (1)
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elements, isotopes
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igneous rocks
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igneous rocks
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plutonic rocks
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pyroclastics
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ignimbrite (1)
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meteorites
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meteorites
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chondrites
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H chondrites (1)
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minerals
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orthosilicates
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nesosilicates
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zircon group
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zircon (1)
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Primary terms
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absolute age (1)
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Asia
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Altai Mountains
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Gorny Altai (1)
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Kuznetsk Alatau (1)
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Altai Russian Federation
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Gorny Altai (1)
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Altai-Sayan region (1)
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Far East
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China
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Sichuan China (1)
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Yangtze Platform (1)
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-
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Salair Ridge (1)
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West Siberia
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Kuznetsk Alatau (1)
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Europe
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Variscides (1)
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faults (1)
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igneous rocks
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plutonic rocks
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granites (1)
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volcanic rocks
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pyroclastics
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ignimbrite (1)
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-
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metals
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alkali metals
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sodium (1)
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-
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meteorites
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stony meteorites
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chondrites
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ordinary chondrites
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H chondrites (1)
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Paleozoic
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Devonian (1)
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Ordovician (1)
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phase equilibria (1)
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plate tectonics (1)
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Precambrian
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upper Precambrian
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Neoproterozoic (2)
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sedimentary rocks
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arkose (1)
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tectonics (1)
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sedimentary rocks
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molasse (1)
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sedimentary rocks
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clastic rocks
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arkose (1)
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The 1126 Ma volcanic event in the Dechang Area, SW Yangtze Block, and its significance
Erratum to “Tectonics and geodynamics of Gorny Altai and adjacent structures of the Altai–Sayan folded area” [Russian Geology and Geophysics 54 (2013) 1250–1271]
Tectonics and geodynamics of Gorny Altai and adjacent structures of the Altai–Sayan folded area
Na behaviour in shock-induced melt phase of the Yanzhuang (H6) chondrite
3-D Evaluation of the Ping Hu Field, East China Sea
Abstract Ping Hu Field, discovered in 1982 in the East China Sea, 365 km offshore China, consists of two structural closures on a complex, faulted anticline. Chinese authorities have planned for the field to provide natural gas to Shanghai in the 21st century. Five wells have been drilled, and more than 2400 km of 2-D and 118 km 2 of 3-D seismic data have been interpreted. Both structures were identified by 2-D data and drilled prior to acquisition of the 3-D seismic data. Interpretation included mapping key reservoirs and fault analysis. Reservoir composition, distribution, and lateral variations were described. These variations were determined by studying geophysical attributes of the data, which included instantaneous amplitude, frequency, phase, and acoustic impedance. Seismic data were inverted to acoustic impedance (density and velocity) and transformed into reservoir parameters. Crossplot regression analyses of petrophysical parameters were performed, and relationships between pairs of values of porosity, acoustic impedance, permeability, and water saturation were derived. An integrated geological–geophysical–reservoir engineering evaluation was required for accurate hydrocarbons-in-place calculations. The interpretation was utilized for field development planning, but implementation has been delayed due to distance from shore relative to field size.