四川北川桂溪地区晚志留亚纪地层的发现
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引用本文:金淳泰,万正权,陈继荣,钱永蓁.1996.四川北川桂溪地区晚志留亚纪地层的发现[J].地球学报,17(1):99-104.
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作者单位
金淳泰 成都地质矿产研究所 
万正权 成都地质矿产研究所 
陈继荣 成都地质矿产研究所 
钱永蓁 成都地质矿产研究所 
中文摘要:四川桂溪地区志田纪地层,于1970年由四川省地质局第二区调队发现,并根据其中所含腕足类Eospirifertingi笼统划归中志留统。1994年,笔者等在这段地层中发现了以牙形石Spathognathoduscrispus,腕足类Retziellauniplicata,床板珊瑚Squameofavosites,Oachyfavosites,Pachycanalicula为代表的晚志留亚纪动物属种,说明该套地层的沉积时限为晚志留亚纪,并可与云南曲靖,四川广元、二郎山、盐边,甘肃迭部等地区相当地层对比。这一发现,对于完善该地区地层系统、研究扬子地台西北缘志日纪古地理演化、海进方向、地质发展史等都具有重要意义。
中文关键词:晚志留亚纪地层  四川桂溪
 
Discovery of Late Silurian Strafa in Guixi, Beichuan, Sichuan
Abstract:The Silurian strata in Guixi area, were discovered originally by the Second Party of Regional Heological Survey,Geologital Bureau of Sichuan in 1970. The strain were referred to the Middle-Upper Silurian Sweepingly based on brachiopod Eospirifer tingi. Authors of this poper found faunas with the hate Silurian characters in the strain through a detailed callection in 1994. The f3unas are represented by conodont Spathognthodus crispus,brachiopod Retziella uniplicata and tabulates:Squameofavosites,Pachyfavosites and Pachycanalicula. These faunas indicate that the strata belong to the ante Silurian and could be correlated with equivalents in Guangyan,Erlangshan and Yanbian,Sichuan,Quging,Yunnan,and Diebu, Gansu. This new discovery is very imPOrtant for study on the paleogeographical evolution, the direction of transgression and regression and geological history in the northwestern margin of the Yangtze Platform.
keywords:Late Silurian strata  Guixi  Sichuan
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