geosyncline
英:[ˌdʒi:əʊ'sɪnklaɪn] 美: [ˌdʒioʊ'sɪnklaɪn]
geosyncline 基本解释
n.地槽;地向斜;
英英释义
Geosyncline
In geology, geosyncline is a term still occasionally used for a subsiding linear trough that was caused by the accumulation of sedimentary rock strata deposited in a basin and subsequently compressed, deformed, and uplifted into a mountain range, with attendant volcanism and plutonism. The filling of a geosyncline with tons of sediment is accompanied in the late stages of deposition by folding, crumpling, and faulting of the deposits.以上来源于:Wikipedia
geosyncline 相关例句
权威例句
GeosynclineGeosynclineGeosynclineDevelopment of the Northern Apennines geosynclineThe Adelaide Geosyncline: Late proterozoic stratigraphy, sedimentation, palaeontology and tectonicsThe Adelaide Geosyncline of South Australia and its significance in Neoproterozoic continental reconLate Precambrian Paleomagnetism of Australia: The Adelaide GeosynclineMultistage ore genesis in the New Zealand geosyncline a history of post-metamorphic lode emplacementSedimentary and Tectonic Processes in the Bengal Deep-Sea Fan and GeosynclineImpact Ejecta Horizon within Late Precambrian Shales, Adelaide Geosyncline, South AustraliaThe Nama Group in South West Africa and Its Relationship to the Pan-African GeosynclineTrace-element geochemistry and sedimentary provinces: A study from the Tasman Geosyncline, AustraliaEvolution of an Early Proterozoic Continental Margin: The Coronation Geosyncline and Associated Aulacogens of the Northwestern Canad...