1) Peng-Guan area
彭灌地区
2) Penglou irrigation area
彭楼引黄灌区
1.
Research and optimization of irrigating mode for Penglou irrigation area with water diverted from Huanghe River;
彭楼引黄灌区灌溉模式优选研究
3) Pengtan-Yangjing Area
彭滩-杨井地区
1.
Physical Properties and Pore Structure of Reservoir Chang 22 in Pengtan-Yangjing Area of Changqing Oilfield;
长庆彭滩-杨井地区长22主力层储层物性及孔隙结构特征研究
4) Pengguan complex
彭灌杂岩
1.
The Pengguan complex,located in the Longmenshan thrust belt,western margin of the Yangtze block,SW China,was formed during the Neoproterozoic.
对位于扬子地块西缘龙门山逆冲推覆构造带中的彭灌杂岩进行了岩石地球化学研究,重点讨论了岩石成因、成岩物质来源及其构造意义。
2.
Pengguan complex as a nappe in the middle Longmen Mountains consists mainly of adamellite, tonalite, moyite and gabbro in the Middle-Late Proterozoic, with an isotopic age of 699-859 Ma by zircon, decollement fault (Yingxiu fault) is a brittle-ductile fault or a strike-slip reverse thrust predominated by brittle deformation.
位于龙门山中段的“彭灌杂岩”推覆体，主要由中晚元古代的二长花岗岩、英云间长岩、钾长花岗岩、辉长岩等组成，用颗粒锆石法测其年龄值为６９９—８５９Ｍａ。
5) Ground water irrigation
地下水灌区
6) landscape drawing of irrigation area
灌区地形图
补充资料：太平洋地区标准会议标准(见太平洋地区标准会议)
太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC
Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条