Hydrodynamic and fluid-inclusion studies of base metal mineralization and hydrocarbon systems in the Paleozoic Anticosti and Maritimes basins, eastern Canada

作     者：Guoxiang Chi Department of Geology, University of Regina, Regina, SK Canada S4S 0A2 E-mail: guoxiang.chi@uregina. ca 

会议名称：《全国包裹体及地质流体学术研讨会》

会议日期：2002年

学科分类：081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 

摘      要：正 The Anticosti Basin, located in the northern part of Gulf of St. Lawrence and centered at Anticosti Island, eastern Canada, is an Early Paleozoic marine basin formed in the eastern margin of the Laurentia continent. It constitutes part of the St. Lawrence Platform. The Maritimes Basin, covering much of the southern part of Gulf of St. Lawrence and surrounding onshore areas, is a Late Paleozoic continental successor basin. It is the uppermost tectonic constituent of the Appalachian Orogen. The Anticosti Basin consists of Cambrian to Lower Ordovician passive margin sediments and Middle Ordovician to Lower Silurian foreland basin sediments, intervened by the Taconian Orogeny in Middle Ordovician. The Maritimes Basin is filled with Upper Devonian to