Results 121 to 130 of about 4,233 (188)
Atmospheric oxygen and methane on the early Earth. [PDF]
Kasting JF, Ji A.
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Dual-layered mantle lithosphere beneath southeastern Canadian Cordillera. [PDF]
Huang S, Gu YJ, Johnston ST.
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Geochemical Characteristics and Organic Matter Enrichment of Mesoproterozoic Shales: Insights from the Cuizhuang Formation, Ordos Basin, North China Craton. [PDF]
Shi Y +12 more
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Integration of geophysical and remote sensing data for structural analysis and delineation of gold, fluorite, and barite mineralization in the Dawi shear belt, Egypt. [PDF]
Eldosouky AM +6 more
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Integrated evaluation of groundwater irrigation suitability using hydrochemical indices and irrigation water quality index (IWQI) in Aksum, Tigray, Ethiopia. [PDF]
Ataklti B, Tesema FW, Berhe BA.
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A regional-scale mobility model for the early hominin occupation of the Lower Omo Valley (Ethiopia). [PDF]
Delagnes A +11 more
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Precambrian Research, 2012
Abstract China contains three major Precambrian blocks, the North China, South China and Tarim cratons, separated and sutured by Phanerozoic orogenic belts. The North China Craton (NCC) contains rocks as old as 3.8 Ga, but is dominated by Neoarchean igneous rocks that were formed during two magmatic events at 2.8–2.7 Ga and 2.55–2.50 Ga.
Guochun Zhao, Peter Cawood
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Abstract China contains three major Precambrian blocks, the North China, South China and Tarim cratons, separated and sutured by Phanerozoic orogenic belts. The North China Craton (NCC) contains rocks as old as 3.8 Ga, but is dominated by Neoarchean igneous rocks that were formed during two magmatic events at 2.8–2.7 Ga and 2.55–2.50 Ga.
Guochun Zhao, Peter Cawood
exaly +4 more sources
Science, 1981
The Precambrian record is interpreted in terms of an evolutionary progression that moves in the direction of increasing continental stability. An early, highly mobile microplate tectonics phase progressed through a more stable, largely intracratonic, ensialic, mobile belt phase to the modern macroplate tectonics phase that involves large, rigid ...
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The Precambrian record is interpreted in terms of an evolutionary progression that moves in the direction of increasing continental stability. An early, highly mobile microplate tectonics phase progressed through a more stable, largely intracratonic, ensialic, mobile belt phase to the modern macroplate tectonics phase that involves large, rigid ...
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Geological Society, London, Memoirs, 1992
Abstract For much of Precambrian time, it is not possible to reconstruct any sort of meaningful palaeogeographies. For this Atlas, therefore, the earliest reconstructions are for Proterozoic intervals and are, of necessity, limited geographically.
R. Anderton, W. Gibbons, P. G. Nicholson
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Abstract For much of Precambrian time, it is not possible to reconstruct any sort of meaningful palaeogeographies. For this Atlas, therefore, the earliest reconstructions are for Proterozoic intervals and are, of necessity, limited geographically.
R. Anderton, W. Gibbons, P. G. Nicholson
openaire +1 more source

