国产极品盛宴视频_久久亚洲精品视频免_亚洲另类 欧美日韩_天天躁中文字幕在线视频


當前位置：希尼爾首頁 > 譯海拾貝 > 翻譯經(jīng)驗 > 海灣大橋工程地質情況簡介Introduction of the geological condition of Qingdao Bay Bridge

 

海灣大橋工程地質情況簡介Introduction of the geological condition of Qingdao Bay Bridge

原創(chuàng)文章：青島希尼爾翻譯公司 http://www.myfavoritepainters.net

2015-3-18

海灣大橋工程地質情況簡介Introduction of the geological condition of Qingdao Bay Bridge

 

  

Introduction of the geological condition of Qingdao Bay Bridge

Through detailed geological survey and reconnaissance over the bridge location and nearby area, the geological “code” in the entire Jiaozhou Bay Area was basically uncovered. The bridge location is divided into four structural units: Jiaozhou – Wangtai Hollow, Jimo – Cangkou Hollow, Xiaozhushan Heave and Qingdao – Laoshan Heave. The lithology at the bridge location is mainly the lava and alloclastic rock of Qingshan Group in cretaceous. To the south and over the Haoguanzhuang sunder, it was the Jiaonan Heave, and the crystallized base is composed of mainly metamophic rock belonging to Archaean and Proterozoic Jiaonan Group; to the east, the crystallized base at the area in the east of Cangkou Sunder is granite in Yanshan Period.

 

The bedrock uncovered during survey was the sedimentary rocks and effusive rock stratum in the cretaceous of Mesozoic Erathem, as well as the intrusion rock of Laoshanchao Unit in the later Yanshan Period.

  

希尼爾翻譯公司