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| 1 | The tectonic uplift of the Hua Shan in the Cenozoic显示文摘Six granite samples were collected from six difference elevation locations at the Hua Shan in a main ridge of the Qinling Mountain. Apatite and zircon separated from these six samples were dated by the fission track technique. An assessment of the Cenozoic uplift or exhumation rate was obtained from the altitude difference of sampling samples dated by fission track, and from the difference of fission track dates of both apatite and zircon for a sample. The preliminary results suggest that the beginning of uplift of the Hua Shan was as early as 68.2 MaBP and the uplift rates for different periods are 0.02-0.19 mm/a (from the elevation difference) or 0.12-0.16 mm/a (from two mineral fission track dates). The average uplift rate is 0.12 mm/a (from the elevation difference) or 0.14 mm/a (from two mineral fission track dates). The uplift of the Hua Shan might accelerate since (17.8±2.0) MaBP, and the average uplift rate is about 0.19 mm/a. | YIN Gongming LU Yanchou ZHAO Hua LI Wanlun LI Li QUO Shilun | 2001 | Chinese Science Bulletin2001，46，19： | 11 |
| 2 | Thickness of calcium carbonate coats on stones of the Heishanxia terraces of the Yellow River and dating of coarse clastic sedimentary geomorphic surfaces显示文摘The calcium carbonate coats on stones developed in soil on the geomorphic surfaces of coarse clastic sediments in arid-semiarid regions contain evident information of age. The thickness of coats can be used not only as a good age indicator for the geomorphic surfaces but also coats themselves can be directly used as dating materials in the ESR method. Through measuring the thickness of carbonate coats on stones in soils on the alluvial terraces in the mouth of the Heishanxia gorge of the Yellow River and ESR dating of layers separated from the carbonate coats, the average of accumulation rates of the thickness of carbonate coats on stones since 1.57 Ma was calculated to be 0.10 mm/ka in the studied area, and a regression equation between carbonate coat thickness and age was also generated. From these research results, ages of T2-T11 terraces of the Yellow River in the studied area were systematically determined, and their values are in turn 18 ka, 94 ka, 139 ka, 215 ka, 305 ka, 410 ka, 495 ka, 742 ka, | Chengqi Xing Gongming Yin Guoyu Ding Yanchou Lu Xuhui Shen Qinjian Tian Zhizhang Chai Kaibo Wei | 2002 | Chinese Science Bulletin2002，47，19： | 7 |
| 3 | Fine grain IRSL and GLSL dating of late Quaternary sediments from North China显示文摘A possible approach to assess the fine grain OSL dating is discussed through comparison of equivalent dose (DE) values and ages obtained by IRSL and GLSL of fine grains for 31 sediment samples from North China. The IRSL and GLSL were measured with the same aliquots for each sample, i.e. shine-down was by 100 s of IRSL (880 nm) followed by 100 s of GLSL (514 nm) on the same discs. The DE values and ages found by IRSL are in good agreement with those by GLSL within 1-2σ for 80% samples, especially for aeolian loess samples. Considering that IRSL from feldspar differs obviously from GLSL dominated from quartz in dose response, thermal stability and optical bleaching characteristic, the agreement between the DE values may be taken as evidence that the two clocks of IRSL and GLSL had been well reset during deposition. The consistent ages of IRSL and GLSL, in turn, may be referred to an indicator to evaluate the fine grain OSL dating of sediments. | ZHAO Hua LU Yanchou CHEN Jie YING Gongming | 2001 | Chinese Science Bulletin2001，46，4： | 5 |
| 4 | Environmental changes recorded in lake sediments for 13000-1000 a B.P. in Beijing area显示文摘The detailed 14 C dating, palynological, carbon isotope and magnetic susceptibility analyses of a paleo swamp record obtained near Beijing show that the succession of climate events in Beijing area is broadly consistent with the climatic behavior in the North Atlantic region during the period from 13 000 to 10 000 a B.P., but with evident local characteristics. A relatively warm and wet episode (11 400\10 950 a B.P.) was intercalated between two dry cold episodes (11 600\11 400 and 10 950\ 10 450 a B.P.). | Lanying Wei Yanchou Lu Jinhui Yin | 1998 | Chinese Science Bulletin1998，43，13： | 2 |
| 5 | Optical dating of Holocene sand dune activities in the Horqin sand-fields in inner Mongolia, China, u- sing the SAR protocol 显示文摘 | Zhao Hua Lu Yanchou Yin Jinhui | 2007 | Quaternary Geochronology Research2007，2，： | 1 |
| 6 | Recuperated OSL dating of fine-grained quartz in Chinese loess显示文摘 | Wang Xulong Lu Yanchou Wintle A G | | 0，，2： | 1 |
| 7 | ReOSL dating of Aeolian and fluvial sediments from Nihewan Basin,northern China and its environmental application显示文摘 | Zhso Hua Lu Yanchou Wang Chengming Chen Jie Liu Jinfeng Mao Hongiiang | | 0，，2： | 1 |
| 8 | Chronology of the stratum containing the skull of the Dali Man显示文摘The field investigations of geomorphology and Quaternary sediment sequences show that the sediment stratigraphic profile containing the skull of the Homo sapiens Daliensis (Dali Man) at Tianshuigou trench, Jiefang Village (109°44’E, 34°52’N ), Dali County, Shaanxi Province, is composed of the loess-paleosol sequence, 17.3 m thick, in the upper part, and the alluvial silts, fine sands and sandy gravels interbedded, 15.4 m thick, in the lower part. There are the well developed layers L1, S1, L2 and S2 in the loess-paleosol sequence of the profile, which are comparable to those of the Luochuan loess section on the basis of magnetic succeptibility measurements and IRSL dating of the loess samples. An alluvial gravel layer, where the skull of the Dali Man was discovered, is in 13 m beneath the bottom of paleosol S2, implying that, the age of the Dali Man must be older than about 247 kaBP when the paleosol S2 began to be developed. The samples of mammal animal tooth and shell fossils from the gravel layer | YIN Gongming ZHAO Hua YIN Jinhui LU Yanchou | 2002 | Chinese Science Bulletin2002，47，15： | 0 |
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