首页> 外文会议>VII Field Conference on the Cambrian Stage Subdivision, Aug 27-Sep 8, 2001, Hunan, Guizhou, Yunnan >CAMBRIAN STRATIGRAPHY AT WANGCUN, HUNAN PROVINCE, CHINA: STRATOTYPES FOR BASES OF THE WANGCUNIAN AND YOUSHUIAN STAGES
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CAMBRIAN STRATIGRAPHY AT WANGCUN, HUNAN PROVINCE, CHINA: STRATOTYPES FOR BASES OF THE WANGCUNIAN AND YOUSHUIAN STAGES

机译:中国湖南望村的寒武纪地层学:望村和尤水阶的地层原型

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Wangcun is an ancient town in southernmost Yongshun County, Hunan Province. The town is an important tourist destination, in part because of its long history and in part because of the attractive riparian scenery nearby along the Mongdonghe River, a branch of the Youshui River. A lengthy Cambrian section is exposed in a roadcut along the highway connecting Wangcun and Luoyixi, on the north bank of the Youshui River (Fengtan Reservoir), about 4 km southeast of Wangcun (Figs. 1, 2). The highway was constructed for the benefit of travelers arriving at the Louyixi railway station, and needing to drive from the railway station to Wangcun. The section is situated on the southeast limb of an undulating syncline, the Liexi-Zhuitun Syncline (Fig. 3). It is one of the major synclines extending through the Jiangnan Slope Belt in northwestern Hunan. Strata exposed in the middle of the syncline include those of the Upper Cambrian through Lower Ordovician. The trend of the structure is north-northeast. Cambrian formations exposed in the Wangcun section include the uppermost part of the Aoxi Formation and the lower and middle parts of the Huaqiao Formation. The Wangcun section serves as the stratotype for both the Wangcunian and the Youshuian stages of the Cambrian, and has recently been the subject of papers by Peng et al. (1995) and Peng and Robison (2000). The Wangcun section is easily accessible by driving west for 48 km on the Zhangjiajie-Yongshun provincial highway from Zhangjiajie to Shiti. Turn left (south) at the T-junction with the Shiti-Wangcun highway, and drive 46 km toward Wangcun until reaching a T-junction with the Wangcun-Luoyixi highway at the east end of the town of Wangcun. At the junction, turn left again (southeast) and follow the highway 5 km to a large bridge over the Fengtan Reservoir (Youshui River), There is another T-junction at the location of the section. The section extends to the northwest along the highway (Fig. 4). The section can be also reached by train travel from either from Zhangjiajie in the north, or from Jishou in the south to Luoyixi; from Luoyixi, it is a 4 km drive to the section. Alternatively, the section can be reached by driving 70 km north from Jishou (Route 3a, Fig. 1).
机译:王村是湖南省永顺县最南端的古镇。该镇是重要的旅游目的地,部分是由于其悠久的历史,部分是由于You水河的分支河-蒙东河沿岸附近迷人的河岸风光。一条长的寒武纪剖面暴露在连接王村和洛衣溪的高速公路上,该道路位于王村东南约4公里的You水河(凤潭水库)北岸(图1、2)。高速公路的建设是为了使旅客到达楼西溪火车站,并需要从火车站开车前往王村。该断面位于起伏斜向线的东南侧,即勒西-垂屯斜向线(图3)。它是贯穿湘西北江南坡带的主要向斜之一。向斜中部裸露的地层包括上寒武统至下奥陶纪。结构的趋势是东北偏北。王村断面暴露的寒武系地层包括奥西组的最上部和华侨组的下部和中部。王村断层是寒武纪王村期和油水期的层型,最近成为彭等人的论文主题。 (1995)和Peng and Robison(2000)。在从张家界到什提的张家界至永顺省道上向西行驶48公里,可轻松抵达王村段。在Shiti-Wangcun公路的丁字路口向左(向南)行驶,向Wangcun行驶46公里,直到在Wangcun镇东端的Wangcun-Luoyixi公路到达T型路口。在路口处,再向左转(东南),然后沿着高速公路行驶5公里,到达凤潭水库((水河)上的一座大桥。该路段的位置还有另一个T型路口。该路段沿公路向西北延伸(图4)。从北部的张家界或南部的吉首到洛衣溪也可以乘火车到达该路段。从罗依溪到此路段有4公里的车程。另外,可以通过从吉首向北行驶70公里(图1a的3a号公路)到达该路段。

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