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'对唐加地区的洋岛型岩石组合进行了野外地质特征、岩浆岩全岩地球化学和锆石U⁃Pb定年研究.唐加地区洋岛型岩石组合的野外地质特征具有典型的“二元结构”,下层为玄武岩基底,上层为灰岩(大理岩)盖层和塌积砾岩,在上部盖层中还可见变质玄武岩夹层和大理岩与绿片岩互层的现象,与“佛得角型”洋岛类似.': [2], '两件玄武岩和一件辉绿玢岩脉的锆石U⁃P定年结果分别为330': [3], 'Ma、310': [4], 'Ma和307': [5], 'Ma,为早石炭世晚期-晚石炭世.': [6], '玄武岩和辉绿玢岩均具有较高的TiO2、P2O5和(Na2O+K2O)含量,稀土元素和微量元素组成与OIB类似,显示明显的Nb、Ta富集,在判别图解中落在OIB和板内玄武岩区域,其岩浆源区可能为尖晶石-石榴子石二辉橄榄岩地幔,熔融深度较小.结合前人研究,初步认为松多古特提斯洋早石炭世晚期可能已经发育了初始洋盆,在早石炭世晚期到晚石炭世为慢/超慢速扩张,形成了具有“佛得角型”洋岛特征的唐加地区洋岛型岩石组合.': [7], '关键词:': [8], '青藏高原': [9], '/': [10, 12, 14, 16, 18], '唐加': [11], '古特提斯洋': [13], '洋岛型岩石组合': [15], 'OIB': [17], '构造地质': [19]}, 'cited_by_api_url': 'https://api.openalex.org/works?filter=cites:W4312588605', 'counts_by_year': [{'year': 2024, 'cited_by_count': 1}], 'updated_date': '2024-09-18T06:23:55.381447', 'created_date': '2023-01-05'}