1.
ESR Stratigraphically Chronological Study of the Gravel Layer in Yangluo Town,Wuhan City
武汉阳逻砾石层ESR地层年代学研究
2.
Cretaceous Magnetostratigraphy of Liupanshan Area and Basin Evolution;
六盘山地区白垩纪磁性地层年代与盆地演化
3.
Magnetostratigraphy Chronology and Sedimentary-tectonic Evolution of the Neogene in the Northern Qaidam Basin
柴北缘新近纪磁性地层年代与沉积构造演化
4.
Magnetostratigraphy of Cretaceous Sediments in Lanzhou-Minhe Basin and Its Implications on the Uplift of the Northern Tibetan Plateau;
兰州—民和盆地早白垩世磁性地层年代与青藏高原北部隆升
5.
Study of the Chronology of Aquifer Strata and the Geochemical Behavior of Uranium of the Underground Brine Along the Southern Coast of Laizhou Bay;
莱州湾南岸含卤地层年代学及卤水中铀的地球化学研究
6.
THE STRATIGRAPHICAL AGES,DIVISION AND CORRELATION OF THE EARLY PRECAMBRIAN IN THE TAIHANGWUTAI AREA,THE YANSHAN AREA AND THE EASTERN SECTOR OF THE YINSHAN MOUNTAINS
太行五台区、燕山区、阴山东段的早前寒武纪地层年代、划分及对比
7.
standard global chronostratigraphic scale
标准世界年代地层表
8.
global chronostratigraphic unit
国际性年代地层单位
9.
informal chronostratigraphic unit
非正式年代地层单位
10.
Study on the OSL Dating in the Loess of Coast (Shelf)
滨海（陆架）黄土释光年代地层研究
11.
Quaternary Lithostratigraphy and Chronostratigraphy Division and Correlation in Kunming Basin;
昆明盆地第四纪岩石地层与年代地层划分与对比
12.
Fission track dating of Cenozoic strata in Linxia Basin
临夏盆地新生代地层裂变径迹年龄测定
13.
CHRONOSTRATIGRAPHY OF PLANKTONIC FORAMINIFERA IN THE YINGGEHAI-QIONGDONGNAN BASIN
南海北部莺琼盆地浮游有孔虫年代地层研究
14.
The Change of Using Stratigraphic Cenozoic Nomenclature in the Field of Stratigraphy in Recent Years
地层学界近年来对新生代地层学名称使用的变化
15.
a layer of rock with a particular composition (especially of fossils); for dating the stratum.
具有特殊成分，尤其是化石的一层岩石；可用来确定地层的年代。
16.
Forming Ages of Early Precambrian Metamorphic Strata in Shandong Province--Proofs of Zircon SHRIMP U-Pb Dating
山东早前寒武纪变质地层形成年代——锆石SHRIMP U-Pb测年的证据
17.
Magnetostratigraphic Age of Pleistocene Loess/Paleosol Sections At Dali, Shaanxi, China
陕西大荔遗址更新世黄土—古土壤剖面磁性地层学年代研究
18.
Particular strata of rocks can be approximately dated according to the presence or absence of certain fossils.
根据特定地层中现存和缺失的化石可以近似的估计年代。