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1)  Hefei-Huangchuan basins
合肥-潢川盆地
2)  Hefei basin
合肥盆地
1.
Research on the geological framework and evolution as well as hydrocarbon prospect of Hefei Basin;
合肥盆地地质格架演化及油气条件分析
2.
Analysis of the Zhuxiang Formation in the eastern part of Hefei Basin by XRD and significance of the results in the light of oil and gas;
合肥盆地东部朱巷组X射线衍射分析及其油气意义
3.
Application of joint-inversion of gravity, magnetic,electric and seismic data to exploration in Hefei basin.;
重磁电震联合反演在合肥盆地勘探中的应用
3)  the Hefei Basin
合肥盆地
1.
A series of parallel thrusting structural belts and foredeep basins were formed in the Hefei Basin of Mesozoic,affected by different stages compression and thrusting orogenesis of Yanshanian Mvt.
合肥盆地是一个以中生界为主体的沉积盆地,受燕山运动Ⅰ幕不同期次挤压逆冲造山的影响,依次形成一系列平行分布的逆冲推覆构造带和前渊盆地。
2.
Based on the data of outcrops and wells on the fringes of the Hefei Basin and the synthetical analyses of stratigraphic characters, organic geochemical indexes and lithofacies paleogeography, the authors believed that the organic abundance of the Liulaobei Formation reached the standard of hydrocarbon source rocks.
依据刘老碑组在合肥盆地周围的露头和钻井资料,通过地层特征、有机地化指标和岩相古地理的综合分析,认为刘老碑组有机质丰度达到烃源岩的要求,母质类型为Ι型干酪根,烃类转化率高,而且泥岩厚度大,总生烃量也大;虽然有机质已经过成熟,但完全可以生气,即处于热裂解成凝析油-湿气阶段,因此提出刘老碑组可作为合肥盆地的气源岩。
3.
Since 1958,the exploration and study of oil and gas in the Hefei Basin was engaged by more than 10 units.
自1958年以来,先后有10余个单位参与过合肥盆地的油气勘探及研究工作,大致经历了三下四上的曲折历程。
4)  Sichuan overlain basin
四川叠合盆地
1.
Sichuan overlain basin is located among the Jiangnan, Qinling-Dabie and Longmen orogenic belts, and at the juncture among ancient Asia, Circum-Pacific and Tethys.
四川叠合盆地三面环山,自东而西夹持于江南、秦岭与龙门山三大山系之间,位于古亚洲、环太平洋与特提斯三大构造域的结合部位;中生代以来,先后经历了海盆、煤盆、陆相广盆、残盆四个盆地世代;盆地沉积充填过程可概括为前陆、坳陷、再生前陆三种基本样式。
5)  The south margin of Hefei Basin
合肥盆地南缘
6)  northeast margin of Hefei basin
合肥盆地东北缘
1.
Cretaceous strata are developed broadly on the northeast margin of Hefei basin with complete sequence upward as early Cretaceous Xizhuang Formation and late Cretaceous Qiuzhuang Formation and Zhangqiao Formation.
合肥盆地东北缘白垩纪地层广泛发育、地层较完整,自下而上为:新庄组、邱庄组和张桥组等3个岩石地层单位。
补充资料:潢川贡面

潢川贡面,历史上称'光州贡面'。此面系清油兑水盐合细面粉,经过拌、揉、发酵、盘条、上架、拉扯、凉晒、截切等十多道工序制成。

据《光州志》载:唐代、潢川已生产挂面,当时'风销华夏,夺魁九州',被人们称为'光州魁面'。传说,到宋朝时,光州州官令工人将这种面去其头尾,取其中间,匀截成20公分左右的长度,用红绿纸卷成园筒形,每筒半斤,作为礼品进献给宫廷,宋仁宗食后,大赞:'美哉,光州贡面'!从此光州精制的筒装挂面,以'贡面'之称闻名于世。

潢川挂面有近千年的历史,生产精制的筒装贡面已有七百年左右,因此制作场坊遍及城乡,所产之面,畅销省内外。解放后,特别是党的十一届三中全会以来,贡面生产蓬勃发展,而且质量越来越好。现在的潢川贡面,条细如丝,中空如管,半斤一筒,色洁如银,包装美观,携带方便,宜于保藏,便于食用。下锅就熟,久不粘汤。清水下,爽利可口;兑汤下,香甜味美。营养价值高。且易于消化。所产数万斤,尚供不应求。 潢川贡面已收入《中国名食录》。

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