Bedrock Geology and Regional Geologic Setting of Coweeta Hydrologic Laboratory in the Eastern Blue Ridge
Bedrock Geology and Regional Geologic Setting of Coweeta Hydrologic Laboratory in the Eastern Blue Ridge
复制标题
蓝岭东部库维塔水文实验室的基岩地质和区域地质环境
DOI：
10.1007/978-1-4612-3732-7_5
复制
发表时间：
1988
影响因子：
5.4
通讯作者：
R. Hatcher
中科院分区：
文献类型：
--
作者：
R. Hatcher
阿巴拉契亚高地是一条更广阔的山脉的最后遗迹，该山脉一度与世界上许多现代较少受到侵蚀的山脉一样高，例如阿尔卑斯山、安第斯山脉和北美科迪勒拉山脉。本章的目的是讨论位于蓝岭东部的 Coweeta 水文实验室的基岩地质，并将其置于蓝岭地质背景中（图 5.1A）。此外，还将讨论第四纪矿床的结构和性质对地形的控制。
The Appalachian Highlands represent the last remnant of a more extensive mountain chain, which at one time was as lofty as many of the modern less eroded chains of the world such as the Alps, Andes, and North American Cordillera. The purpose of this chapter is to discuss the bedrock geology of Coweeta Hydrologic Laboratory, which is situated in the eastern Blue Ridge, and place it into the context of Blue Ridge geology (Figure 5.1A). In addition, some discussion of control of topography by structure and the nature of the Quaternary deposits will be made.