1) Late Carboniferous
晚石炭世
1.
Depositional Environment in Late Carboniferous-Early Permian in Southern Hetian Area of Southwest Tarim Basin．;
塔西南和田南部晚石炭世-早二叠世沉积环境
2.
Approach to Sedimentary Environment of Late Carboniferous-Permian in Junggar basin;
准噶尔盆地晚石炭世和二叠纪沉积环境
3.
Brachiopod diversity and sedimentary environments of the Late Carboniferous and early Early Permian in Jungar,Inner Mongolia;
内蒙古准格尔旗晚石炭世一早二叠世早期腕足类物种多样性与沉积环境
2) Upper Carboniferous
晚石炭世
1.
The siliceous rocks of Qiergusitao Group of Upper Carboniferous(C2q) was widely distributed in the southwest of Dabancheng, Xinjiang Uygur Autonomous Region.
新疆乌鲁木齐达坂城西南晚石炭世奇尔古斯套组(C2q)硅质岩分布极为广泛,通过野外地质填图及矿产调查过程中的详细观察和硅质岩岩石学、常量元素、稀土元素和微量元素的分析,认为这些硅质岩的成因复杂,以火山成因及热水成因为主,同时也有生物化学成因。
3) middle-Late carboniferous
中晚石炭世
4) late Late Carboniferous
晚石炭世晚期
1.
On the basis of the study on the flora characteristic of the late Late Carboniferous and early Early Permian in the Helan Mountains, the palaeoecology study on this flora has been analyzed.
在综合研究了贺兰山北段晚石炭世晚期和早二叠世早期植物群的特征和性质的基础上 ,对此植物群进行了古生态学方面的分析研究。
2.
The coal bearing strata and flora of late Late Carboniferous and early Early Permian in the Shabatai area of Shizuishan, Ningxia are studied.
对宁夏石嘴山沙巴台地区晚石炭世晚期—早二叠世早期含煤地层和植物群进行了研究，共鉴定植物化石１２属１７种，划分了２个植物化石组合，即晚石炭世晚期ＬｅｐｉｄｏｄｅｎｄｒｏｎｓｚｅｉａｎｕｍＮｅｕｒｏｐｔｅｒｉｓｏｖａｔａ组合和早二叠世早期ＴａｅｎｉｏｐｔｅｒｉｓｍｕｃｒｏｎａｔａＡｎｎｕｌａｒｉａｏｒｉｅｎｔａｌｉｓ组合，其代表地层为晚石炭世晚期的太原组和早二叠世早期的山西组；此外，还讨论了含煤地层植物群的特征和时代。
3.
The fossil plants studied in this paper were collected from the late Late Carboniferous and early Early Permian strata of Datong coalfield, Shanxi Province.
对山西大同煤田晚石炭世晚期和早二叠世早期植物化石进行了研究，共鉴定植物化石２１属４８种，划分２个植物组合，讨论了植物群的特征和时代；此外，还论证了本区晚石炭世晚期和早二叠世早期植物群指示的古气候条
5) Late Carboniferous granite
晚石炭世花岗岩
1.
Petrographic evidence of magma mixing of Late Carboniferous granite in the Xiao Hinggan Mountains, China and its geological implications;
小兴安岭晚石炭世花岗岩岩浆混合作用的岩相学证据及其地质意义
6) Upper Carboniferous Dalaan Stage
晚石炭世达拉阶
1.
The age of the stratum within these conodonts fossils can be confirmed in the Upper Carboniferous Dalaan Stage.
1∶5万区域地质矿产调查于东天山库姆塔格沙垄地区康古尔塔格深大断裂北侧灰岩中,发现了Streptognathodus suberectus,Idiognathoides sinuata等牙形石,确认其地质时代为晚石炭世达拉阶,该套地层归属哈尔里克地层小区底坎儿组,具有弧后盆地建造特色。
补充资料：夏晚寻于政世置酒赋韵
【诗文】：
聊从嘉遁所，酌醴共抽簪。以兹山水地，留连风月心。
长榆落照尽，高柳暮蝉吟。一返桃源路，别后难追寻。
【注释】：
【出处】：
全唐诗：卷39_3
聊从嘉遁所，酌醴共抽簪。以兹山水地，留连风月心。
长榆落照尽，高柳暮蝉吟。一返桃源路，别后难追寻。
【注释】：
【出处】：
全唐诗：卷39_3
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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