-
摘要:
山东黄土是沿海地区轨道尺度气候变化和海平面变化的重要记录，冰期大量接收从出露的渤海沉积物风蚀而来的粉尘而与黄土高原等地的内陆黄土在物源上有很大不同，因此具有重要的研究价值。但与黄土高原黄土相比，山东黄土得到的关注较少，研究程度较低。年代学是开展风成沉积古气候重建的基础，由于受研究方法的制约，山东黄土的年代学研究仍然有很多问题亟待解决。重点总结山东黄土在年代学研究方面的进展，通过分析现有年代的可靠性，提出山东黄土年代学研究存在的问题；认为年代学研究应当成为现阶段山东黄土的研究重点，可通过光释光测年(或者结合26Al/10Be埋藏测年)来建立可靠的年代学框架，为气候变化和地貌演化研究奠定基础；同时围绕年代学研究的核心，提出了山东黄土目前值得关注的几个重要的研究方向。
Abstract:Owing to the large amount of dust input from the exposed Bohai shelf during the glacier periods, the loess in Shandong region has quite different material sources from those on the Chinese Loess Plateau and other inland regions. The Shandong loess is a very important archive for climate and sea level changes in the coastal areas in orbital time-scales. However, it has not raised enough attention so far comparing to the loess at the Loess Plateau. Even though there have been increased input in recent years, they are still less than enough. As we are aware, chronology is the basis for paleoenvironmental reconstruction and geomorphologic studies and the major concern of geologists, it must be prioritized in the future research. After summarizing the published ages of Shandong loess, their reliability is analyzed and some problems about chronology of the Shandong loess proposed in this paper. We suggest that the chronology studies on Shandong loess should focus more on establishment of reliable chronological frameworks with optically stimulated luminescence dating (or combined with 26Al /10Be dating) as the major method. A few important associated scientific questions and suggestions concerning Shandong loess are also proposed in this paper.
-
-
表 1 山东部分黄土剖面释光年代数据及参数
Table 1. Luminescence dating results and parameters of loess in Shandong
剖面 深度/m K/% Th/10-6 U/10-6 含水量% 等效剂量(Gy) 剂量率(Gy/ka) 年代/ka 方法 矿物 粒径/μm 可靠性 LQ[43] 1 2.07 8.73 1.95 109 4.17 26.1 OSL 石英 可靠 2 2.23 7.82 1.65 120 4.13 29.1 OSL 石英 可靠 3 2.11 9.83 1.92 160 4.35 36.7 OSL 石英 基本可靠 4 2.09 9.76 2.05 180 4.45 40.4 OSL 石英 可能低估 5 2.13 11.4 2.31 200 4.75 42.1 OSL 石英 可能低估 6 2.22 9.9 1.67 248 4.42 56.1 OSL 石英 可能低估 7 2.3 10.2 2.09 355 4.61 77 OSL 石英 低估 GG[43] 0.5 2.2 14.3 2.2 50.3±3.8 4.9±0.5 10.2±0.8 OSL 石英 可靠 2.1 2.4 29.6 3.3 >400 7.7±0.8 >50 OSL 石英 低估 BC[43] 2 2.3 11.4 2 103.7±3.5 4.5±0.5 23.1±1.9 OSL 石英 可靠 3.5 2.3 10.9 1.9 119.5±4.4 4.4±0.5 27.6±3.5 OSL 石英 可靠 5 2.4 10.6 1.8 112.5±4.8 4.4±0.5 25.6±3.9 OSL 石英 可靠 6.5 2.5 11.4 1.9 213.5±17.5 4.6±0.5 46.3±5.5 OSL 石英 可能低估 XLZ[13] 3.5 2.54 131.62±3.15 4.91 26.83±0.64 OSL 石英 4~11 可靠 7.5 3.09 145.00±3.01 4.17 34.80±0.72 OSL 石英 4~11 可靠 TJ[13] 1 2.66 102.62±1.59 4.93 20.73±0.32 OSL 石英 4~11 可靠 6.6 2.54 299.05±9.75 4.67 64.01±2.09 OSL 石英 4~11 低估 BHC[43] 1 2.5 8.8 1.7 49.8±5.8 4.2±0.4 11.8±1.4 OSL 石英 90~300 可靠 2.7 2.4 9.3 1.7 50.9±3.4 4.2±0.4 12.1±0.8 OSL 石英 90~300 可靠 4.2 2.3 10.3 1.9 106.4±3.7 4.0±0.4 24.6±0.9 OSL 石英 90~300 可靠 6.2 2.3 9.5 1.7 80.2±3.8 4.1±0.4 19.4±0.9 OSL 石英 90~300 可靠 YS[43] 0.5 2.2 14.1 1.8 41.5±4.0 4.7±0.5 8.9±0.9 OSL 石英 90~300 可靠 2.2 2.2 29.7 1.5 57.8±4.0 7.1±0.7 8.0±0.6 OSL 石英 90~300 可靠 3.6 2.2 10.6 1.9 76.9±4.2 4.2±0.4 18.1±1.0 OSL 石英 90~300 可靠 XJY[44] 0.8 2.4 11.5 2 66.2±4.1 4.6±0.5 14.4±1.0 OSL 石英 90~300 可靠 2.5 2.2 11.3 1.9 92.2±4.4 4.3±0.4 21.4±1.1 OSL 石英 90~300 可靠 3.9 2.1 10.1 1.9 211.8±10.8 4.1±0.4 51.8±2.6 OSL 石英 90~300 可能低估 ZL[40] 1 1.38 9.08 2.47 82.9±1.0 3.1±0.4 26.9±3.6 OSL 石英 90~300 可靠 2.2 1.03 5.99 2.55 130.9±2.9 2.7±0.3 47.5±1.6 OSL 石英 90~300 可靠 2.4 1.09 6.39 2.51 141.5±5.3 2.8±0.6 50.5±1.9 OSL 石英 90~300 可靠 6.6 1.77 10.26 2.56 354.5±29.3 3.5±0.4 101.2±8.8 OSL 石英 90~300 低估 8.2 1.14 7.27 2.77 308.9±23.1 3.0±0.3 106.5±7.7 OSL 石英 90~300 低估 9.1 1.71 9.71 2.75 391.1±7.3 3.5±0.4 112.5±8.3 OSL 石英 90~300 低估 10.6 1.53 9.26 2.62 366.7±41.6 3.3±0.3 111.9±12.4 OSL 石英 90~300 低估 11.6 0.98 8.41 2.82 291.7±40.6 2.9±0.2 99.7±13.6 OSL 石英 90~300 低估 12.9 0.84 6.23 2.82 >400 2.7±0.3 >100 OSL 石英 90~300 低估 14 0.91 6.93 2.83 >400 2.8±0.3 >100 OSL 石英 90~300 低估 LGZ[20] 1.4 2.4 135.91±13.9 5.725 23.74±2.44 OSL 石英 4~11 可靠 5.7 2.62 386.24±25.6 5.256 73.49±4.87 OSL 石英 4~11 低估 QZ[11] 2.1 2.18 10.64±0.23 2.09±0.21 22 33.0±1.0 3.40±0.11 9.7±0.4 OSL 石英 可靠 7.1 1.76 10.17±0.22 1.92±0.20 22 219.4±11.2 2.93±0.10 74.8±4.6 OSL 石英 可能低估 10.5 2.04 11.55±0.25 2.06±0.22 22 608.0±3.0 3.29±0.11 185.1±6.5 OSL 石英 低估 BX[38] 0.5 2.4 12.5 2.4 11 4.4±0.5 4.4±0.5 1.0±0.1 OSL 石英 可靠 1.1 2.3 14.9 3 8 68.7±5.0 5.2±0.6 13.2±1.0 OSL 石英 可靠 2.1 2.4 11.2 2.1 15 62.7±15.1 4.4±0.5 14.1±3.4 OSL 石英 可靠 3.1 2.5 12.8 2.4 15 69.5±5.6 4.8±0.5 14.4±1.5 OSL 石英 可靠 4.1 2.7 13.9 2.3 20 84.7±7.6 5.0±0.5 17.1±1.6 OSL 石英 可靠 5.1 2.6 13.6 2.3 21 95.7±13.3 5.0±0.5 19.4±2.7 OSL 石英 可靠 6.1 2.4 11.5 2.1 15 112.7±15.4 4.7±0.5 24.1±3.3 OSL 石英 可靠 7.6 2.5 10.5 1.9 21 131.7±5.8 4.4±0.4 30.0±3.5 OSL 石英 可靠 9.6 2.3 12.7 2.3 17 159.7±5.6 4.6±0.5 34.8±1.2 OSL 石英 基本可靠 13.1 2.6 13.9 2.7 23 203.1±8.8 5.1±0.5 39.2±1.8 OSL 石英 可能低估 QZ[9] L1底 1.61 12.82 1.24 4.2 209.3 3.07 68±5 TL 未知 L2底 1.7 19.89 3.7 4.9 1 046.5 4.6 227±18 TL 不可信 L3底 2.21 23 0.55 3.8 1 524.9 4.82 313±25 TL 不可信 L5底 1.75 21.7 1.69 3.8 2 272.4 5.15 441±35 TL 不可信 L6下 1.81 16.63 1.17 3.4 2 810.2 4.8 585±46 TL 不可信 L9上 1.96 14.76 1.62 4.6 3 049.8 3.84 793±64 TL 不可信 淄河店[9] L1底 1.55 13.2 2.76 4.5 508.3 3.54 143±11 TL 不可信 L2底 1.64 13.5 1.61 4.6 897 3.7 242±19 TL 不可信 龙桥[9] L5底 1.7 9.3 2.04 4.5 5554.8 3.28 474±38 TL 不可信 山旺[9] L2底 2.28 13.28 2.6 3.2 890 4.18 213±15 TL 不可信 L3底 1.8 8.76 2.25 3.3 1 042.8 3.22 324±28 TL 不可信 下朱潘[9] L3上 1.98 16.8 1.38 5 926.9 3.76 250±19 TL 不可信 铜井[9] L8顶 1.91 8.96 2.01 3.8 2 780.8 3.84 724±58 TL 不可信 长岛[9] L2上 1.6 11.54 1.96 5.2 508.3 3.2 158±12 TL 不可信 
下载: 导出CSV
-
[1] 刘东生.黄土与环境[J].西安交通大学学报:社会科学版, 2002, 22(4):7-12. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200306014
LIU Dongsheng. Loess and environment[J]. Journal of Xi'an Jiaotong University(Social Sciences), 2002, 22(4):7-12. http://d.old.wanfangdata.com.cn/Periodical/dsjyj200306014
[2] 陈一萌, 曾宪光.中国西北与华北地区末次冰期黄土气候记录的对比研究[J].中国沙漠, 2009, 29(6):1075-1080. http://d.old.wanfangdata.com.cn/Periodical/zgsm200906011
CHEN Yimeng, ZENG Xianguang. Comparative study of climate changes recorded in loess strata both in northwest China and northern China during the last glacial period[J].Journal of Desert Research, 2009, 29(6):1075-1080. http://d.old.wanfangdata.com.cn/Periodical/zgsm200906011
[3] 牛光明, 强明瑞, 宋磊, 等.5 000 a来柴达木盆地东南缘风成沉积记录的冬季风演化[J].中国沙漠, 2010, 30(5):29-37. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgsm201005007
NIU Guangming, QIANG Mingrui, SONG Lei, et al. Change of eastern Asian winter monsoon recorded by aeolian deposits over the past 5 000 years at the southeastern margin of Qaidam Basin[J].Journal of Desert Research, 2010, 30(5):29-37. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgsm201005007
[4] Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22Myr ago inferred from loess deposits in China[J].Nature, 2002, 416(6877):159-163. doi: 10.1038/416159a
[5] 赵松龄.晚更新世末期中国陆架沙漠化及其衍生沉积的研究[J].海洋与湖沼, 1991, 22(3):285-293. http://www.cnki.com.cn/Article/CJFD1991-HYFZ199103014.htm
ZHAO Songling. China shelf sea desertization and its derived deposits during the last stage of late Pleistocene[J]. Oceanologia et Limnologia Sinica, 1991, 22(3):285-293. http://www.cnki.com.cn/Article/CJFD1991-HYFZ199103014.htm
[6] 刘东生.第四纪环境[M].北京:科学出版社, 1997.
LIU Dongsheng. Quaternary Environments[M]. Beijing:Science Press, 1997.
[7] 曹家欣, 李培英, 石宁.山东庙岛群岛的黄土[J].中国科学B辑, 1987, 17(10):1116-1123. http://d.old.wanfangdata.com.cn/Periodical/hykx200812010
CAO Jiaxin, LI Peiying, SHI Ning. Loess of Miaodao island in Shandong[J]. Science in China(B), 1987, 17(10):1116-1123. http://d.old.wanfangdata.com.cn/Periodical/hykx200812010
[8] 张祖陆.渤海莱州湾南岸平原黄土阜地貌及其古地理意义[J].地理学报, 1995, 50(5):465-470. http://www.cnki.com.cn/Article/CJFDTotal-DLXB505.009.htm
ZHANG Zulu. Loess mounds on the Laizhou Bay plain south of Bohai Sea and their paleogeographic implication[J]. Acta Geographica Sinica, 1995, 50(5):465-470. http://www.cnki.com.cn/Article/CJFDTotal-DLXB505.009.htm
[9] 郑洪汉, 朱照宇, 黄宝林, 等.山东半岛及苏皖北部黄土地层年代学研究[J].海洋地质与第四纪地质, 1994, 14(1):64-68. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ401.006.htm
ZHENG Honghan, ZHU Zhaoyu, HUANG Baolin, et al. A study on loess geochronology of Shandong peninsula and northern part of Jiangsu and Anhui provinces[J]. Marine Geology and Quaternary Geology, 1994, 14(1):64-68. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ401.006.htm
[10] 刘乐军, 李培英, 王永吉.鲁中黄土粒度特征及其成因探讨[J].海洋地质与第四纪地质, 2000, 20(1):81-86. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz200001013
LIU Lejun, LI Peiying, WANG Yongji. The grain-size properties and genesis of the loess in central Shandong province[J].Marine Geology and Quaternary Geology, 2000, 20(1):81-86. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz200001013
[11] 彭淑贞, 朱丽君, 肖国桥, 等.山东青州黄土的地层年代及其物质来源研究[J].干旱区地理, 2010, 33(6):947-953. http://d.old.wanfangdata.com.cn/Periodical/ghqdl201006014
PENG Shuzhen, ZHU Lijun, XIAO Guoqiao. Magnetostratigraphy and provenance of the Qingzhou loess in Shandong Province[J]. Arid Land Geography, 2010, 33(6):947-953. http://d.old.wanfangdata.com.cn/Periodical/ghqdl201006014
[12] 于洪军.中国东部陆架黄土成因的新探索[J].第四纪研究, 1999, 19(4):367-372. http://www.cnki.com.cn/Article/CJFDTotal-DSJJ199904008.htm
YU Hongjun. A new exploration on the origin of loess in the shelf area of the eastern China seas[J]. Quaternary Sciences, 1999, 19(4):367-372. http://www.cnki.com.cn/Article/CJFDTotal-DSJJ199904008.htm
[13] 徐树建.晚第四纪我国风尘堆积的区域对比研究[M].济南:山东人民出版社, 2012.
XU Shujian. Regional Comparative Studies of the Late Quaternary Eolian Deposits in China[M]. Jinan:Shandong People′s Publishing House, 2012.
[14] 李徐生, 杨达源, 鹿化煜.镇江下蜀黄土粒度特征及其成因初探[J].海洋地质与第四纪地质, 2001, 21(1):25-32. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz200101005
LI Xusheng, YANG Dayuan, LU Huayu. Grain-size features and genesis of the Xiashu loess in Zhenjiang[J]. Marine Geology and Quaternary Geology, 2001, 21(1):25-32. http://d.old.wanfangdata.com.cn/Periodical/hydzydsjdz200101005
[15] 张祖陆, 辛良杰, 聂晓红.山东地区黄土研究综述[J].地理科学, 2004, 24(6):746-752. doi: 10.3969/j.issn.1000-0690.2004.06.018
ZHANG Zulu, XIN Liangjie, NIE Xiaohong. A summary of loessial researches in Shandong[J]. Scientia Geographica Sinica, 2004, 24(6):746-752. doi: 10.3969/j.issn.1000-0690.2004.06.018
[16] 彭淑贞, 高志东, 吴秀平, 等.山东青州地区黄土的粒度组成及成因分析[J].地质力学学报, 2007, 13(4):315-321. doi: 10.3969/j.issn.1006-6616.2007.04.004
PENG Shuzhen, GAO Zhidong, WU Xiuping, et al. Grain-size distribution and genesis of loess in the Qingzhou area, Shandong[J]. Journal of Geomechanics, 2007, 13(4):315-321. doi: 10.3969/j.issn.1006-6616.2007.04.004
[17] 张祖陆, 辛良杰, 姜鲁光, 等.山东济南张夏黄土堆积及成因分析[J].古地理学报, 2005, 7(1):98-106. doi: 10.3969/j.issn.1671-1505.2005.01.009
ZHANG Zulu, XIN Liangjie, JIANG Luguang, et al. Sedimentary characteristics and genetic analysis of Zhangxia Loess in Jinan, Shandong Province[J]. Journal of Palaeogeography, 2005, 7(1):98-106. doi: 10.3969/j.issn.1671-1505.2005.01.009
[18] 徐树建.山东庙岛群岛黄土的粒度特征及其环境意义[J].海洋科学, 2008, 32(12):60-63. http://d.old.wanfangdata.com.cn/Periodical/hykx200812010
XU Shujian. Grain size characteristics and its indications of loess in Miaodao Islands, Shandong Province[J]. Marine Sciences, 2008, 32(12):60-63. http://d.old.wanfangdata.com.cn/Periodical/hykx200812010
[19] 安芷生.洛川黄土地层学[J].第四纪研究, 1989, 9(2):155-168. doi: 10.3321/j.issn:1001-7410.1989.02.006
AN Zhisheng. Loess stratigraphy in Luochuan of China[J].Quaternary Sciences, 1989, 9(2):155-168. doi: 10.3321/j.issn:1001-7410.1989.02.006
[20] 徐树建, 王涛.蓬莱黄土剖面光释光年代学及其沉积特征研究[J].中国沙漠, 2011, 31(2):295-301. http://d.old.wanfangdata.com.cn/Conference/7449570
XU Shujian, WANG Tao. Optically stimulated luminescence dating and sedimentary characteristics of loess section at Penglai in Shandong province[J]. Journal of Desert Research, 2011, 31(2):295-301. http://d.old.wanfangdata.com.cn/Conference/7449570
[21] 孙洪艳, 李志祥, 田明中.第四纪测年研究新进展[J].地质力学学报, 2003, 9(4):371-378. doi: 10.3969/j.issn.1006-6616.2003.04.009
SUN Hongyan, LI Zhixiang, TIAN Mingzhong. New progress in Quaternary dating research[J]. Journal of Geomechanics, 2003, 9(4):371-378. doi: 10.3969/j.issn.1006-6616.2003.04.009
[22] Heller F, Liu T S. Magnetostratigraphical dating of loess deposits in China[J]. Nature, 1982, 300(5891):431-433. doi: 10.1038/300431a0
[23] 刘东生, 安芷生.洛川北韩寨黄土磁性地层学的初步研究[J].地球化学, 1984, 13(2):134-137. doi: 10.3321/j.issn:0379-1726.1984.02.005
LIU Dongsheng, AN Zhisheng. A preliminary magnetostratigraphic study of the Beihanzhai loess section[J]. Geochimica, 1984, 13(2):134-137. doi: 10.3321/j.issn:0379-1726.1984.02.005
[24] Rutter N W, Ding Z L, Evans M E, et al. Magnetostratigraphy of the Baoji Loess-paleosol Section in the North-Central China Loess Plateau[J].Quaternary International, 1991, 7(8):97-102. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-1040-6182(90)90043-4/
[25] Yu L P, Lai Z P. OSL chronology and palaeoclimatic implications of aeolian sediments in the eastern Qaidam Basin of the northeastern Qinghai-Tibetan Plateau[J].Palaeogeography Palaeoclimatology Palaeoecology, 2012, 337-338(4):120-129. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=6e1751aecdd59818db0a20e65be72f62
[26] Madsen A T, Murray A S. Optically stimulated luminescence dating of young sediments: A review[J]. Geomorphology, 2009, 109(1-2):3-16. doi: 10.1016/j.geomorph.2008.08.020
[27] Yu L P, Lai Z P. Holocene climate change inferred from stratigraphy and OSL chronology of aeolian sediments in the Qaidam Basin, northeastern Qinghai-Tibetan Plateau[J]. Quaternary Research, 2014, 81(3):488-499. doi: 10.1016/j.yqres.2013.09.006
[28] Yu L P, Lai Z P, An P, et al. Aeolian sediments evolution controlled by fluvial processes, climate change and human activities since LGM in the Qaidam Basin, Qinghai-Tibetan Plateau[J]. Quaternary International, 2015, 372(6):23-32. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=4d28ed40d630bf63df94df7f213095cc
[29] Liu X J, Lai Z P, Madsen D, et al. Lake level variations of Qinghai Lake in northeastern Qinghai-Tibetan Plateau since 3.7 ka based on OSL dating[J]. Quaternary International, 2011, 236(1-2):57-64. doi: 10.1016/j.quaint.2010.08.009
[30] Buylaert J P, Vandenberghe D, Murray A S, et al. Luminescence dating of old (>70 ka) Chinese loess: A comparison of single-aliquot OSL and IRSL techniques[J].Quaternary Geochronology, 2007, 2(1-4):9-14. doi: 10.1016/j.quageo.2006.05.028
[31] Buylaert J P, Murray A S, Huot S. Optical dating of an Eemian site in Northern Russia using K-feldspar[J].Radiation Measurements, 2008, 43(2-6):715-720. doi: 10.1016/j.radmeas.2008.01.027
[32] Rink W J, Bartoll J, Schwarcz H, et al. Testing the reliability of ESR dating of optically exposed buried quartz sediments[J]. Radiation Measurements, 2007, 42(10):1618-1626. doi: 10.1016/j.radmeas.2007.09.005
[33] 刘春茹, 尹功明, 韩非, 等.石英ESR测年法在第四纪陆相沉积物测年中的应用[J].第四纪研究, 2016, 36(5):1236-1245. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201605018
LIU Cunru, YIN Gongming, HAN Fei, et al. ESR dating methodology and its application in dating Quaternary terrestrial sediments[J]. Quaternary Sciences, 2016, 36(5):1236-1245. http://d.old.wanfangdata.com.cn/Periodical/dsjyj201605018
[34] Grün R. The DATA program for the calculation of ESR age estimates on tooth enamel[J]. Quaternary Geochronology, 2009, 4(3):31-232. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=c98acf64e21c715218fe06f3b777461d
[35] Granger D E, Kirchner J W, Finkel R C. Quaternary downcutting rate of the New River, Virginia, measured from differential decay of cosmogenic 26Al and 10Be in cave-deposited alluvium[J]. Geology, 1997, 25(2):107-110. http://d.old.wanfangdata.com.cn/NSTLQK/10.1130-0091-7613(1997)025-0107-QDROTN-2.3.CO%3b2/
[36] 孙政, 沈冠军, 赖忠平. 26Al/10Be等时线埋藏测年法基本原理与应用简介[J].盐湖研究, 2012, 20(2):66-72. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yhyj201202011
SUN Zheng, SHEN Guanjun, LAI Zhongping. Introduction to basic principles and applications of isochron 26 Al/10Be burial dating method[J].Journal of Salt Lake Research, 2012, 20(2):66-72. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yhyj201202011
[37] 沈冠军, 邵庆丰, Darryl E GRANGER. 26Al/10Be埋藏测年法及其在我国早期人类遗址年代研究中的应用[J].人类学学报, 2009, 28(3):292-299. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=rlxxb200903007
SHEN Guanjun, SHAO Qingfeng, Darryl E GRANGER. 26Al/10Be burial dating and its potential in dating early hominid sites in China[J]. Acta Anthropologica Sinica, 2009, 28(3):292-299. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=rlxxb200903007
[38] 徐树建, 丁新潮, 倪志超.山东埠西黄土剖面沉积特征及古气候环境意义[J].地理学报, 2014, 69(11):1707-1717. doi: 10.11821/dlxb201411011
XU Shujian, DING Xinchao, NI Zhichao. The sedimentary characteristics of Buxi loess profile in Shandong Province and their paleoclimatic and palaeoenvironment significance[J]. Acta Geographica Sinica, 2014, 69(11):1707-1717. doi: 10.11821/dlxb201411011
[39] Murray A S, Wintle A G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol[J]. Radiation Measurements, 2000, 32(1):57-73. doi: 10.1016/S1350-4487(99)00253-X
[40] 李强.山东潍坊朱里黄土剖面光释光年代及环境意义[D].山东: 山东师范大学, 2014.
LI Qiang. Loess chronology and environmental significance of Weifang Zhuli profile in Shandong province[D]. Shandong: Shandong Normal University, 2014.
[41] 徐树建, 李强, 付信花, 等.胶莱盆地北部风尘堆积物光释光年代序列研究[J].干旱区资源与环境, 2015, 29(5):48-52. http://d.old.wanfangdata.com.cn/Periodical/ghqzyyhj201505009
XU Shujian, LI Qiang, FU Xinhua, et al. Study on the OSL chronosequence of eolian deposits in the northern of Jiaolai Basin[J]. Journal of Arid Land Resources and Environment, 2015, 29(5):48-52. http://d.old.wanfangdata.com.cn/Periodical/ghqzyyhj201505009
[42] 丁新潮, 曹文, 徐树建, 等.山东平阴黄土剖面稀土元素特征及对物源的指示意义[J].干旱区资源与环境, 2015, 29(9):188-192. http://d.old.wanfangdata.com.cn/Periodical/ghqzyyhj201509033
DING Xinchao, CAO Wen, XU Shujian, et al. Characteristics of rare earth elements in Pingyin loess profile, Shandong Province and its implications for provenance[J]. Journal of Arid Land Resources and Environment, 2015, 29(9):188-192. http://d.old.wanfangdata.com.cn/Periodical/ghqzyyhj201509033
[43] 倪志超.山东庙岛群岛黄土光释光年代及物源探讨[D].山东: 山东师范大学, 2015.
NI Zhichao. Optically Stimulated Luminescence Dating and the provenance analysis of Loess in Miaodao Islands, Shandong Province[D]. Shandong: Shandong Normal University, 2015.
[44] Xu S J, Ding X C, Yu L P, et al. Palaeoclimatic implications of aeolian sediments on the Miaodao Islands, Bohai Sea, East China, based on OSL dating and proxies[J].Aeolian Research, 2015, 19(12):259-266. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=c35ea3d9fe8713e98b494be9be4f293c
[45] 卢演俦, 赵华.陕西渭南介子村黄土的热释光测年[J].地质论评, 1991, 37(4):356-362. doi: 10.3321/j.issn:0371-5736.1991.04.008
LU Yanchou, ZHAO Hua. Thermoluminescence dating of the late Quaternary loess-paleosoil sequence at the Jiezicun section, Weinan county, Shanxi province[J]. Geological Review, 1991, 37(4):356-362. doi: 10.3321/j.issn:0371-5736.1991.04.008
[46] Lai Z P, Fan A C. Examining quartz OSL age underestimation for loess samples from Luochuan in the Chinese Loess Plateau[J].Geochronometria, 2014, 41(1):57-64. doi: 10.2478/s13386-013-0138-1
[47] Chapot M S, Roberts H M, Duller G A T, et al. A comparison of natural- and laboratory-generated dose response curves for quartz optically stimulated luminescence signals from Chinese Loess[J]. Radiation Measurements, 2012, 47(11-12):1045-1052. doi: 10.1016/j.radmeas.2012.09.001
[48] Buylaert J P, Murray A S, Vandenberghe D, et al. Optical dating of Chinese loess using sand-sized quartz:Establishing a time frame for Late Pleistocene climate changes in the western part of the Chinese Loess Plateau[J]. Quatemary Geochronology, 2008, 3(1-2):99-113. doi: 10.1016/j.quageo.2007.05.003
[49] Li B, Jacobs Z, Roberts R, et al. Review and assessment of the potential of post-IR IRSL dating methods to circumvent the problem of anomalous fading in feldspar luminescence[J]. Geochronometria, 2014, 41(3):178-201. doi: 10.2478/s13386-013-0160-3
[50] Li B, Li S H. Luminescence dating of Chinese loess beyond 130ka using the non-fading signal from K-feldspar[J]. Quatemary Geochronology, 2012, 10(7):24-31. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=979e97b1b37f6355fe99378ab9af3ec4
-
图(2)
表(1)
计量
- 文章访问数: 1490
- PDF下载数: 61
- 施引文献: 0