1.
Discovery of the Middle Devonian spores from Baimianxia Formation of Sanhuashi Group,Xixiang-Shiquan region,South Qinling,China and its geological significance
南秦岭西乡—石泉地区三花石群白勉峡组中泥盆世孢子化石的发现及其地层意义
2.
much-branched pink with flowers in clusters; closely related to sweet William.
成群开花的多树枝石竹；非常接近于须苞石竹。
3.
Hydrothermal Synthesis of 3D Flowerlike Boehmite Microstructures
水热合成三维花状薄水铝石微观结构
4.
FRESHWATER APUS FOSSIL GROUP IN JURASSIC AND TRIAS-SIC IN XINJIANG.
新疆侏罗纪、三叠纪淡水鲎虫化石群
5.
Seen from some distance away, the different shades in color on the cliff appear like a herd of horse.
从远处看，岩石上不同的花纹像是一群马。
6.
Preliminarily exploring the characteristics of Neolitsea homi lantha in Shilin vegetation restoration area
石林植被恢复地团花新木姜子种群特征初探
7.
Study on Dominant Community of Disanthus cercidifolius subsp. longipes from Mountain Sanqingshan of Jiangxi Province
江西省三清山长柄双花木优势群落研究
8.
The granitic rocks in Zhuluke area, Western Liaoning, emplaced during Late Hercynian-Indosinian cycle, with Rb-Sr isochronal dating age of 226.8～260 Ma.
朱碌科地区花岗质岩石侵位时间为二叠－三叠纪。
9.
Environmental Significance of Glauconite in Funing Group(Paleogene), Tungtai Depression, Kiangsu Province
苏北东台拗陷下第三系阜宁群的海录石
10.
RESEARCH ON TERTIARY PALYNOFLORA FROM THE FOSSIL HILL FORMATION OF KING GEORGE ISLAND,ANTARCTICA
南极乔治王岛第三纪化石山组的孢粉植物群
11.
Preliminary Study of Cultivated Vegetation Reconstruction in Sanlidong Gangue Waste Lands
三里洞矸石废弃地人工植被群落构建初探
12.
granite pilllar and picture
花岗石柱及花岗石画
13.
Determination of the Content of Huperzine A in Huperzia serrata from Three Different Populations of Huaihua Region,Hunan Province
怀化地区蛇足石杉三个居群的石杉碱甲含量的测定
14.
EARLIEST TRIASSIC AMMONOID FAUNAS FROM JIANGSU AND ZHEJIANG AND THEIR BEARING ON THE DEFINITION OF PERMO-TRIASSIC BOUNDARY
论苏、浙一带三叠纪最早期的菊石群及二叠系—三叠系界线的定义
15.
LATE MIDDLE AND EARLY LATE CAMBRIAN CONODONTS FROM HUAYUAN,HUNAN
湖南花垣中寒武世晚期至晚寒武世早期牙形石动物群(英文)
16.
Presentation of Ethnic Identity: A Case Study of the Hua Miao in Simenkan;
族群身份的论述:石门坎花苗知识分子的个案研究
17.
Education and Ethnic Identification;
教育与民族认同:贵州石门坎花苗族群认同的建构
18.
Wenquan granite is composed of two end-member rocks, one is the host rock of the acid end-member, and the other is the microgranular mafic enclave.
温泉花岗岩体由酸性端元的寄主岩石和暗色微细粒镁铁质包体群及基性岩墙群组成。