[1] 陈伟光,张虎男,李子权,张福来. 1987. 琼北北海组地层沉积、发育的几个问题. 热带地理, 7(3): 268-275. [Chen W G,Zhang H N,Li Z Q,Zhang F L.1987. Some problems of deposition and development of the Beihai formation in Northern Hainan Island. Tropical Geography, 7(3): 268-275] [2] 龚正权. 2010. 晚更新世以来闽东沿海风沙沉积的古季风变化记录研究. 福建师范大学硕士学位论文,31-35. [Gong Z Q.2010. Study of Paleo-monsoon Recorded by Aeolian Deposit in the Coastal Area of East Fujian since the Late Pleistocene. Master’s Thesis of Fujian Normal University,31-35] [3] 胡凡根,李志忠,靳建辉,陈秀玲,夏菁,王贤立. 2012. 福建晋江海岸带老红砂多期发育模式初步研究. 第四纪研究, 32(6): 1207-1220. [Hu F G,Li Z Z,Jin J H Chen X L,Xia J,Wang X L.2012. Aprimary research on multiphase development pattern of Old red sand in Jinjiang coast of Southeast Fujian,Quaternary Sciences, 32(6): 1207-1220] [4] 黄镇国,张伟强,陈俊鸿,刘瑞华,何正翀. 1996. 中国南方红色风化壳. 北京: 海洋出版社, 1-312. [Huang Z G,Zhang W Q,Chen J H,Liu R H,He Z C.1996. Weathering Crusts in South China. Beijing: China Ocean Press, 1-312] [5] 金志敏,廖炳良,吴正. 1994. 华南沿海“老红砂”红化作用研究. 科学通报, 39(12): 1122-1124. [Jin Z M,Liao B L,Wu Z.1994. Research on laterization of the “Old Red Sand”along the coasts of South China. Chinese Science Bulletin, 39(12): 1122-1124] [6] 靳建辉,李志忠,雷国良,凌智永,姜峰,申健玲,刘秀铭. 2017. 华南老红砂沉积年代学及其环境意义: 以福建青峰老红砂为例. 地理科学, 37(2): 301-310. [Jin J H,Li Z Z,Lei G L,Ling Z Y,Jiang F,Shen J L,Liu X M.2017. Chronology and environmental significance of Old Red Sand in South China: Take the Old Red Sand in Qingfeng,Fujian as an example. Scientia Geographica Sinica, 37(2): 301-310] [7] 申健玲,李志忠,靳建辉,邓涛,姜峰,苑秀全,于晓莉,赖海成. 2016. 福建海坛岛青峰老红砂旋回沉积的粒度特征及其古环境意义. 中国沙漠, 36(4): 972-982. [Shen J L,Li Z Z,Jin J H,Deng T,Jiang F,Yuan X Q,Yu X L,Lai H C.2016. Grain-size characteristics and the paleoenvironmental significance of the cyclically deposited “Old Red Sand”in Qingfeng,Haitan Island,Fujian,China. Journal of Desert Research, 36(4): 972-982] [8] 温小浩,李保生,孟洁,杨庆江,郑琰明,牛东风,王丰年,蔡瑜杭. 2015.150~20kaB.P.福建东部平潭岛海岸风成沉积的粒度特征及其环境意义. 中国沙漠, 35(6): 1473-1482. [Wen X H,Li B S,Meng J,Yang Q J,Zheng Y M,Niu D F,Wang F N,Cai Y H.2015. Grain size characteristics of coatsal aeolian sediments in the Pingtan Island of Fujian,China,and their implications for the paleoenvironment from 150ka BP to 20 ka BP. Journal of Desert Research, 35(6): 1473-1482] [9] 吴正,黄山,胡守真,吴克刚,金志敏,朱膺. 1995. 华南海岸风沙地貌研究. 北京: 科学出版社,114-118. [Wu Z,Huang S,Hu S Z,Wu K G,Jin Z M,Zhu Y.1995. Research on the Landforms of the Wind-drift Sand in South China Coast. Beijing: Science Press,114-118] [10] 吴正,王为. 1997. 华南沿海老红砂的成因与古地理环境. 中国科学: D辑, 27(6): 537-542. [Wu Z,Wang W.1997. The formation and paleogeographical environment of old red sand in South China. Science in China: Series D, 27(6): 537-542] [11] 吴正,王为,谭惠忠,许峰宇. 2000. 闽南粤西沿海老红砂的沉积年代. 科学通报, 45(5): 533-537. [Wu Z,Wang W,Tan H Z,Xu F Y.2000. The age of the “Old Red Sands”on the coasts of South Fujian and West Guangdong,China. Chinese Science Bulletin, 45(5): 1216-1221. [12] 杨传成,陈杰,张克旗,刘进峰,王昌盛,雷生学. 2007. 水成相沉积物细颗粒石英光释光综合生长曲线的建立与应用. 地震地质, 29(2): 402-411. [Yang C C,Chen J,Zhang K Q,Liu J F,Wang C S,Lei S X.2007. Standardized growth curves(SGC)for optical dating of fine-grained quartz from water lain sediments. Seismology and Geology, 29(2): 402-411] [13] 杨光复,韩有松,张铭汉,王少青. 1982. 关于胶东半岛“柳夼红层”沉积特征及其成因的探讨. 海洋与湖沼, 13(3): 231-242. [Yang G F,Han Y S,Zhang M H,Wang S Q.1982. A discussion about the sedimentary character and the origin of “Liukuang Red Bed”in the east Shandong peninsula. Oceanologia et Limnologia Sinica, 13(3): 231-242] [14] 杨树康. 1982. 华南沿海第四纪地层划分和海岸升降. 热带海洋学报, 1(1): 25-38. [Yang S K.1982. Division of the coastal quaternary layers and coastal subsidence-elevation in the south China. Tropic Oceanology,1(1): 25-38] [15] 俞鸣同,张红艳,龚正权,陈有喜,王佳韡,张熠,胡绍洁,吴惠. 2014. 福建平潭青峰老红砂中季风组分以及形成期研究. 地理科学, 34(3): 352-357. [Yu M T,Zhang H Y,Gong Z Q,Chen Y X,Wang J W,Zhang Y,Hu S J,Wu H.2014. The monsoon components in Qingfeng old red sands and their formation epoch,Pingtan island,Fujian Province. Scientia Geographica Sinica, 34(3): 352-357] [16] 袁宝印,夏正楷,李保生,乔彦松,顾兆炎,张家富,许冰,黄慰文,曾荣树. 2008. 中国南方红土年代地层学与地层划分问题. 第四纪研究, 28(1): 1-13. [Yuan B Y,Xia Z K,Li B S,Qiao Y S,Gu Z Y,Zhang J F,Xu B,Huang W W,Zeng R S.2008. Chronostratigraphy and stratigraphic division of red soil in southern China. Quaternaty Sciences, 28(1): 1-13] [17] 曾从盛,陈居成,吴幼恭. 1999a. 闽东南沿海老红砂沉积地层与形成时代. 中国沙漠, 19(4): 338-342. [Zeng C S,Chen J C,Wu Y G.1999a. Sedimentary stratum and forming age of the “old red sand”along the coast of Southeast Fujian. Journal of Desert Research, 19(4): 338-342] [18] 曾从盛,陈居成,吴幼恭. 1999b.闽东南沿海老红砂研究. 北京: 地质出版社,35-39. [Zeng C S,Chen J C,Wu Y G.1999b. Research of Old Red Sand in Southeast Fujian. Beijing: Geological Publishing House,35-39] [19] 张家富,袁宝印,周力平. 2007. 福建晋江“老红砂”的释光年代学及对南方第四纪沉积物释光测年的指示意义. 科学通报, 52(22): 2646-2654. [Zhang J F,Yuan B Y,Zhou L P.2007. Luminescence chronology of “Old Red Sand”in Jinjiang and its implication for optical dating of sediments in South China. Chines Science Bulletin, 52(22): 2646-2654] [20] 张静然. 2010. 末次间冰期以来季风边缘区黄旗海高湖面释光年代学及其环境意义. 江西师范大学硕士学位论文,29-31. [Zhang J R.2010. Luminescence Chronology for High Lake Levels and Its Palaeoenvironmental Implications of Huangqihai Lake in Inner Mongolia since the Last Interglacial. Master’s Thesis of Jiangxi Normal University,29-31] [21] Aitken M J.1998. An introduction to optical dating: The Dating of Quaternary Sediments by the Use of Photon-Stimulated Luminescence. Oxford: Oxford University Press. [22] Bøtter-Jensen L,Mckeever S W S,Wintle A G.2003. Optically Stimulated Luminescence Dosimetry. Elsevier. [23] Burbidge C I,Duller G A T,Roberts H M.2006. De determination for young samples using the standardised OSL response of coarse-grain quartz. Radiation Measurements, 41(3): 278-288. [24] Chen G Q,Yi L,Xu X Y,Yu H J,Cao J R,Su Q,Yang L H,Xu Y H,Ge J Y,Lai Z P.2013. Testing the standardized growth curve(SGC)to OSL dating: Coastal sediments from the south Bohai Sea,China. Geochronometria, 40(2): 101-112. [25] Choi J H,Duller G A T, Wintle A G.2006. Analysis of quartz LM-OSL curves. Ancient TL, 24(1): 9-20. [26] Choi J H,Kim J W,Murray A S,Hong D G,Chang H W,Cheong C S.2009. OSL dating of marine terrace sediments on the southeastern coast of Korea with implications for Quaternary tectonics. Quaternary International, 199(1-2): 3-14. [27] Murray-Wallace C V,Jones B G,Nghi T,Price D M,Vinh V V,Tinh T N,Nanson G C.2002. Thermoluminescence ages for a reworked coastal barrier,southeastern Vietnam: A preliminary report. Journal of Asian Earth Sciences, 20(5): 535-548. [28] Durcan J A,Duller G A T.2011. The fast ratio: A rapid measure for testing the dominance of the fast component in the initial OSL signal from quartz. Radiation Measurements, 46(10): 1065-1072. [29] Gardner R A M,Pye K.1981. Nature,origin and palaeoenvironmental significance of red coastal and desert dune sands. Progress in Physical Geography, 5(4): 514-534. [30] Gueniot B,Munier-Lamy C,Berthelin J.1988. Geochemical behavior of uranium in soils,part Ⅰ. Influence of pedogenetic processes on the distribution of uranium in aerated soils. Journal of Geochemical Exploration, 31(1): 21-37. [31] Huntley D J,Hutton J T,Prescott J R.1993. The stranded beach-dune sequence of south-east South Australia: A test of thermoluminescence dating,0-800ka. Quaternary Science Reviews, 12(1): 1-20. [32] Jain M,Murray A S,Bøtter-Jensen L.2003. Characterisation of blue-light stimulated luminescence components in different quartz samples: Implications for dose measurement. Radiation Measurements, 37(4-5): 441-449. [33] Jayangondaperumal R,Murari M K,Sivasubramanian P,Chandrasekar N,Singhvi A K.2012. Luminescence dating of fluvial and coastal red sediments in the SE coast,India,and implication for paleoenvironmental changes and dune reddening. Quaternary Research, 77(3): 468-481. [34] Jin J H,Li Z Z,Huang Y M,Jiang F,Fan X C,Ling Z Y,Cheng Y,Xu X L.2017. Chronology of a late Neolithic Age site near the southern coastal region of Fujian,China. The Holocene, 27(2): 1265-1272. [35] Lai Z P.2006. Testing the use of an OSL standardised growth curve(SGC)for De determination on quartz from the Chinese Loess Plateau. Radiation Measurements, 41(1): 9-16. [36] Lai Z P,Brückner H.2008. Effects of Feldspar Contamination on Equivalent dose and the Shape of Growth Curve for OSL of Silt-Sized Quartz Extracted from Chinese Loess. Geochronometria, 30: 49-53. [37] Lai Z P,Brückner H,Zöller L,Fülling A.2007. Existence of a common growth curve for silt-sized quartz OSL of loess from different continents. Radiation Measurements, 42(9): 1432-1440. [38] Lai Z P,Brückner H,Fülling A,Zöller L.2008. Effects of thermal treatment on the growth curve shape for OSL of quartz extracted from Chinese loess. Radiation Measurements, 43(2-6): 763-766. [39] Li B,Jacobs Z,Roberts R G.2016. Investigation of the applicability of standardised growth curves for OSL dating of quartz from Haua Fteah cave,Libya. Quaternary Geochronology, 35: 1-15. [40] Long H,Lai Z P,Fan Q S,Sun Y J,Liu X J.2010. Applicability of a quartz OSL standardised growth curve for De determination up to 400 Gy for lacustrine sediments from the Qaidam Basin of the Qinghai-Tibetan Plateau. Quaternary Geochronology, 5(2): 212-217. [41] Murray A S,Wintle A G.2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements, 32(1): 57-73. [42] Murray A S,Wintle A G.2003. The single aliquot regenerative dose protocol: Potential for improvements in reliability. Radiation Measurements, 37(4): 377-381. [43] Prescott J R,Hutton J T.1994. Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations. Radiation Measurements, 23(2-3): 497-500. [44] Roberts H M.2007. Assessing the effectiveness of the double-SAR protocol in isolating a luminescence signal dominated by quartz. Radiation Measurements,42(10): 1627-1636. [45] Roberts H M,Duller G A T.2004. Standardised growth curves for optical dating of sediment using multiple-grain aliquots. Radiation Measurements, 38(2): 241-252. [46] Shen Z,Mauz B.2011. Estimating the equivalent dose of late Pleistocene fine silt quartz from the Lower Mississippi Valley using a standardized OSL growth curve. Radiation Measurements, 46(8): 649-654. [47] Singarayer J S,Bailey R M.2003. Further investigations of the quartz optically stimulated luminescence components using linear modulation. Radiation Measurements, 37(4-5): 451-458. [48] Smith B W,Rhodes E J.1994. Charge movements in quartz and their relevance to optical dating. Radiation Measurements, 23(2-3): 329-333. [49] Srivastava P,Sangode S J,Parmar N,Meshram D C,Priyanka J,Singhvi A K.2016. Mineral magnetic characteristics of the late Quaternary coastal red sands of Bheemuni,East Coast(India). Journal of Applied Geophysics, 134: 77-88. [50] Stevens T,Armitage S J,Lu H Y,Thomas D S G.2007. Examining the potential of high sampling resolution OSL dating of Chinese loess. Quaternary Geochronology, 2(1-4): 15-22. [51] Telfer M W,Bateman M. D,Carr A S,Chase B M.2008. Testing the applicability of a standardized growth curve(SGC)for quartz OSL dating: Kalahari dunes,South African coastal dunes and Florida dune cordons. Quaternary Geochronology, 3(1-2): 137-142. [52] Tsakalos E,Dimitriou E,Kazantzaki M,Anagnostou C,Christodoulakis J,Filippaki E.2018. Testing optically stimulated luminescence dating on sand-sized quartz of deltaic deposits from the Sperchios delta plain,central Greece. Journal of Palaeogeography, 7(2): 130-145. [53] Thomsen K J,Jain M,Murray A S,Denby P M,Roy N,Bøtter-Jensen L.2008. Minimizing feldspar OSL contamination in quartz UV-OSL using pulsed blue stimulation. Radiation Measurements, 43(2): 752-757. [54] Wintle A G,Murray A S.2000. Quartz OSL: Effects of thermal treatment and their relevance to laboratory dating procedures. Radiation Measurements, 32(5): 387-400. [55] Wintle A G,Murray A S.2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements, 41(4): 369-391. [56] Yang L H,Lai Z P,Long H,Long H,Zhang J R.2011. Construction of a quartz OSL standardised growth curve(SGC)for aeolian samples from the Horqin dunefield in northeastern China. Geochronometria, 38(4): 391-396. [57] Zhao H,Lu Y,Yin J.2007. Optical dating of Holocene sand dune activities in the Horqin sand-fields in inner Mongolia,China,using the SAR protocol. Quaternary Geochronology, 2(1-4): 29-33. |