本文選題：CORS　切入點：山東地殼運動　出處：《測繪科學》2017年07期 　論文類型：期刊論文

【摘要】：建立高精度的地殼運動速度場模型是實現區(qū)域大地基準動態(tài)維持,反映地面形變,保障基礎設施工程建設的重要途徑。針對點位分布密集、精度可靠和多年連續(xù)重復觀測等準確獲取區(qū)域地殼運動速度場模型的關鍵問題,通過對山東及周邊省份2010年1月—2015年11月連續(xù)近6a的130座連續(xù)運行參考站點在ITRF2008框架下進行處理,獲取時間序列。首次完整建立了山東省地殼運動速度場模型。通過模型分析表明:水平方向,山東省地殼整體向東南方向運動,平均速率為34.3mm/a,運動方向為SE110.25°;垂直方向,魯中山區(qū)及膠東半島地區(qū)地殼較為穩(wěn)定,魯北、魯西等華北平原地區(qū)存在顯著沉降,最大沉降量位于廣饒漏斗區(qū),年沉降量81.6mm/a。
[Abstract]:Establishing a high precision velocity field model of crustal movement is an important way to realize the dynamic maintenance of regional geodetic datum, to reflect ground deformation and to ensure the construction of infrastructure engineering. The key problems in accurately obtaining the velocity field model of regional crustal movement, such as reliable accuracy and continuous and repeated observation for many years, are discussed. Through the processing of 130 continuous operation reference stations in Shandong and its surrounding provinces from January 2010 to November 2015 for nearly 6 consecutive years, under the framework of ITRF2008, The velocity field model of crustal movement in Shandong Province is established for the first time. The results of model analysis show that the horizontal direction, the whole crust of Shandong Province moves southeast, the average velocity is 34.3 mm / a, the direction of movement is SE110.25 擄, the vertical direction is vertical. The crust is stable in Shandong Central Mountain area and Jiaodong Peninsula, and there is significant subsidence in North China Plain, such as North Shandong and West Shandong. The maximum subsidence is located in Guangrao funnel area, and the annual subsidence is 81.6 mm / a.
【作者單位】： 山東省國土測繪院;山東城市建設職業(yè)學院;山東省泰山氣象站;
【基金】：教育部中央高�；究蒲袠I(yè)務費專項資金項目 中國科學院遙感與數字地球研究所項目 四川省應急測繪保障與地質災害監(jiān)測工程技術研究中心開放研究基金項目(K2014B003) 國家博士后基金項目(2011M501400)
【分類號】：P227;P228.4
，

本文編號：1584768