1) late Changhsingian

长兴期晚期
1.
The warm-and cool-water mixed fauna indicates ocean current influenced biota in the late Changhsingian in South China.
深水分子与浅水分子混生的特征与长兴期晚期断杉剖面位于深水盆地相的边缘,并且离浅水碳酸盐岩台地较近的古地理位置一致;暖水分子与凉水分子混生暗示扬子海盆当时可能存在洋流活动。
2) the late Changxingian

晚长兴期
3) Changxing age

长兴期
1.
Study On lithofacies Paleogeography of Changxing Age of Late Permian in the South of Anhui;
皖南晚二叠世长兴期岩相古地理研究
2.
This paper deals wiht the forming characteristics of these coal- forming models, their spacial distribution conditions and typical coal layers in Wujiapin age and Changxing age, it points out that the tidal flat type was th.
文章阐述了这些成煤模式在吴家坪期和长兴期形成的特征,分布状况,以及代表煤层,指出潮坪型是广西晚二叠世时期最主要的成煤模式。
5) Changhsingian

长兴期
1.
The Upper Permian Changhsingian succession is well exposed in the northeast Beibei, Chongqing City.
重庆北碚地区晚二叠世长兴期地层出露良好,剖面位于北碚代家沟东北部,经过详细调查研究,在厚度为110。
2.
The research shows the abundance and diversity are closely related to sea level changes of Changhsingian age at the Meishan D Section.
结果表明:煤山D剖面长兴组的放射虫动物群的相对丰度、简单分异度与长兴期海平面变化具有耦合性:放射虫丰度、分异度较大的层位基本对应于长兴早期和长兴晚期2次最大海侵事件发生的层位。
3.
A well preserved late Changhsingian Radiolarian assemblage has been discovered from a carbonate siliceous series of the Changhsing Formation in Liuqiao area, Guangxi, South China.
广西南宁南部柳桥地区的长兴组上部硅质岩中保存着精美的长兴期晚期放射虫动物群 ,共有 2 4属 3 9种 ,其中 3个新种 ,其中以 L atentifistularia最为常见 ,其次是 Albaillellidae和 Entactiniidae,属于二叠纪晚期的 N eoal-baillella optima组合。
6) Changxingian

长兴期
1.
A Changxingian smaller foraminifera fauna (non fusulinid foraminifera) from Sidazhai section in Ziyun County, Guizhou Province, southwest China is reported here.
首次报道了产自贵州紫云四大寨剖面长兴期的有孔虫动物群 ,共计有 9属 2 2种。
2.
Here studied are the features of paleoecology and braehiopod fauna from the Changxingian of Huayingshan, Sichuan, with a correlation of limestone facies Changxingian brachiopod faunas between Huayingshan and other regions.
四川华蓥山地区二叠纪长兴期地层中共采获腕足动物90种44属,其中10新种,1新亚种。
补充资料:长兴
1.复姓。汉有长兴渠。见《资治通鉴.汉安帝延光四年》。
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