黄龙组原称“黄龙石灰岩”。中石炭世。最初命名地点在中国江苏镇江石马庙。因本组石灰岩构成了龙潭镇以西的黄龙山主体，故名。本组分布于宁镇山脉及南方各省，岩性稳定，分下、上两部：下部，灰白色、浅红灰色厚层白云岩含燧石结核；上部灰白色、微红色厚层质纯灰岩，富含蜒类化石原小纺锤蜓、小纺锤蜓及珊瑚、腕足类化石黄龙多壁管珊瑚、莫斯科分喙贝等。厚约30—180米。本组与下石炭统在桂、黔、滇东呈整合接触，在苏南、垸南呈假整合接触，在桂中呈角度不整合或假整合接触。本组大致与四川、贵州的威宁群及华北的本溪组相当。
出露于桐庐冷坞的上石炭统黄龙组、船山组和下二叠统栖霞组、丁家山组，总厚932.3米。
The Huanglong, Chuanshan formation of Upper Carboniferous and the Qixia, Dingjiashan formation of Lower Permian, outcropping in Tonglu-Lengwu, have a total thickness of 932.3 meters.
并与浙江长兴、杭州、常山地区的老虎洞组、黄龙组剖面进行了生物地层和岩石地层的划分对比。
Moreover, the biostratigraphic and lithostratigraphic correlation has been made between this section and the section of the two formations in Changxing, Hangzhou and Changshan in Zhejiang.
方法：将阿片类药物相关便秘68例患者随机分为治疗组(新加黄龙汤)和对照组(麻仁软胶囊)进行3周对比观察。
Methods: Opioid-related constipation in 68 patients were randomly divided into treatment group (new Huanglong soup) and the control group (hemp seed soft capsule) for 3 weeks Observation.
应用推荐