A geologic history of the north-central Appalachians, part 2: the Appalachian basin from the Silurian through the carboniferous

Rodger T.Faill

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A geologic history of the north-central Appalachians, part 2: the Appalachian basin from the Silurian through the carboniferous

机译：阿巴拉契亚中北部的地质历史，第2部分：从志留纪到石炭纪的阿巴拉契亚盆地

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The north-central Appalachians occupy a critical posi- tion within the 3000+km-long Appalachian orogen, lying southwest of the boundary between the central and northern Appalachians (CNAB). The one-billion-year-long history of tectonic activity in the north- central Appalachians includes the assembly and breakup of a late Proterozoic supercontinent, the creation and evolution of the Appala- chains orogen during the Paleozoic, and the Mesoxoic transformation of the active orogen into a passive margin during Pangea's disassembly.

机译：中北部的阿巴拉契亚山脉位于中部和北部阿巴拉契亚山脉（CNAB）边界西南的3000多公里长的阿巴拉契亚造山带中，处于一个关键位置。阿巴拉契亚中北部的构造活动已有十亿年的历史，包括晚元古生代超大陆的组装和破裂，古生代期间阿巴拉链造山带的形成和演化以及活动古道的中生代转变。在Pangea拆卸过程中造山带进入被动边缘。

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《American Journal of Science》 |1997年第7期|p.729-761|共33页
作者
Rodger T.Faill;
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收录信息美国《科学引文索引》(SCI);
原文格式 PDF
正文语种 eng
中图分类一般工业技术;地质学;
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A geologic history of the north-central Appalachians, part 2: the Appalachian basin from the Silurian through the carboniferous

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