Mate logo
主页
应用程序
MacMac + SafariiOSiPhone + iPadChromeGoogle ChromeFirefoxMozilla FirefoxOperaOperaEdgeMicrosoft Edge
博客帮助中心联系我们登录
应用程序

iPhone + iPad

帮助中心, 新版本推出通知, 下载

Mac + Safari

帮助中心, 新版本推出通知, 下载

Google Chrome

帮助中心, 下载

Mozilla Firefox

帮助中心, 下载

Opera

帮助中心, 下载

Microsoft Edge

帮助中心, 下载
支持
下载帮助中心支持的语言申请退款恢复密码恢复序列码隐私政策
保持联系
联系我们Twitter博客
语言
免费服务
网页翻译器在线翻译器动词词形变化Der Die Das 查询用法示例WordsDefinitionIdioms
Mate logo
主页
应用程序
MacMac + SafariiOSiPhone + iPadChromeGoogle ChromeFirefoxMozilla FirefoxOperaOperaEdgeMicrosoft Edge
博客帮助中心联系我们登录
应用程序

iPhone + iPad

帮助中心, 新版本推出通知, 下载

Mac + Safari

帮助中心, 新版本推出通知, 下载

Google Chrome

帮助中心, 下载

Mozilla Firefox

帮助中心, 下载

Opera

帮助中心, 下载

Microsoft Edge

帮助中心, 下载
支持
下载帮助中心支持的语言申请退款恢复密码恢复序列码隐私政策
保持联系
联系我们Twitter博客
语言
免费服务
网页翻译器在线翻译器动词词形变化Der Die Das 查询用法示例WordsDefinitionIdioms

“graben”在英语中的释义

noun

  1. (geology) An elongated block of the Earth's crust, bounded by faults, that has dropped relative to the surrounding area.

    • 1959, Robert G. Yates, George A. Thompson, Geology and Quicksilver Deposits of the Terlingua District, Texas, U. S. Geological Survey, Professional Paper 312, page 49, The magnitude and shape of the large grabens strongly suggest that, when they formed, material much more mobile than ordinary rocks was present at a depth no greater than a few miles.
    • 1997, Jean-Marie Rouchy, 2: Paleogene Continental Rift System of Western Europe, Georges Busson, B. Charlotte Schreiber (editors), Sedimentary Deposition in Rift and Foreland Basins in France and Spain (Paleogene and Lower Neogene), page 83, Migration of the subsidence axis has been revealed by the detailed sedimentological studies in most of these grabens, particularly in the Bresse basin (Curial 1986; Moretto 1986/1987) and in Manosque-Forcalquier.
    • 2015, C. F. Burgess, et al., Chapter 35: The Structural and Stratigraphic Evolution of Lake Tanganyika: A Case Study of Continental Rifting, W. Manspeizer (editor), Triassic-Jurassic Rifting: Continental Breakup and the Origin of the Atlantic Ocean and Passive Margins, Part A, page 866, These distinct zones of strike-slip or scissor faulting which separate adjacent half-grabens were termed interbasinal ridges and hinged highs by Rosendahl et al. (1986).