Natural saturation of OSL and TT-OSL signals of quartz grains from Nilotic origin

[1]  N. Porat,et al.  Geo-chronological context of the open-air Acheulian site at Nahal Hesi, northwestern Negev, Israel , 2017 .

[2]  J. Hublin,et al.  The first Neanderthal remains from an open-air Middle Palaeolithic site in the Levant , 2017, Scientific Reports.

[3]  A. Wintle,et al.  Optically stimulated luminescence signals from quartz: A review , 2017 .

[4]  N. Porat,et al.  Rujm el-Hiri: The Monument in the Landscape1 , 2017 .

[5]  Jakob Wallinga,et al.  Violet stimulated luminescence dating of quartz from Luochuan (Chinese loess plateau) : Agreement with independent chronology up to ∼600 ka , 2016 .

[6]  Jie Chen,et al.  Stability of fine‐grained TT‐OSL and post‐IR IRSL signals from a c. 1 Ma sequence of aeolian and lacustrine deposits from the Nihewan Basin (northern China) , 2016 .

[7]  Zhongping Lai,et al.  Natural and laboratory TT-OSL dose response curves: Testing the lifetime of the TT-OSL signal in nature , 2016 .

[8]  N. Porat,et al.  Aggradation–incision transition in arid environments at the end of the Pleistocene: An example from the Negev Highlands, southern Israel , 2016 .

[9]  A. Murray,et al.  Fundamental investigations of natural and laboratory generated SAR dose response curves for quartz OSL in the high dose range , 2015 .

[10]  R. Amit,et al.  Provenance of the Various Grain-Size Fractions in the Negev Loess and Potential changes in Major dust Sources to the Eastern Mediterranean , 2015, Quaternary Research.

[11]  M. Bar-Matthews,et al.  Accounting for kinetic isotope effects in Soreq Cave (Israel) speleothems , 2014 .

[12]  N. Porat,et al.  Geological setting and age of the Middle Paleolithic site of Nahal Mahanayeem Outlet (Upper Jordan Valley, Israel) , 2014 .

[13]  Zhongping Lai,et al.  Examining quartz OSL age underestimation for loess samples from Luochuan in the Chinese Loess Plateau , 2014 .

[14]  J. Wallinga,et al.  Towards dating Quaternary sediments using the quartz Violet Stimulated Luminescence (VSL) signal , 2013 .

[15]  N. Porat,et al.  Origin of the Sinai–Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history , 2013 .

[16]  N. Porat,et al.  From mass‐wasting to slope stabilization – putting constrains on a tectonically induced transition in slope erosion mode: a case study in the Judea Hills, Israel , 2013 .

[17]  Zhongping Lai,et al.  A comparison of natural- and laboratory-generated dose response curves for quartz optically stimulated luminescence signals from Chinese Loess , 2012 .

[18]  A. Murray,et al.  A comparison of TT-OSL and post-IR IRSL dating of coastal deposits on Cap Bon peninsula, north-eastern Tunisia , 2012 .

[19]  A. Matmon,et al.  Constant cosmogenic nuclide concentrations in sand supplied from the Nile River over the past 2.5 m.y. , 2012 .

[20]  C. Cosma,et al.  Optical dating of Romanian loess: A comparison between silt-sized and sand-sized quartz , 2011 .

[21]  Z. Shen,et al.  Source-trap characterization of thermally transferred OSL in quartz , 2011 .

[22]  R. Amit The role of the Nile in initiating a massive dust influx to the Negev late in the middle Pleistocene , 2011 .

[23]  F. Preusser,et al.  Underestimation of fine grain quartz OSL dating towards the Eemian: Comparison with palynostratigraphy from Azzano Decimo, northeastern Italy , 2010 .

[24]  A. Wintle,et al.  Improving the TT-OSL SAR protocol through source trap characterisation , 2010 .

[25]  N. Porat,et al.  A simplified SAR protocol for TT-OSL , 2009 .

[26]  A. Murray,et al.  Testing the potential of an elevated temperature IRSL signal from K-feldspar , 2009 .

[27]  Onn Crouvi,et al.  Sand dunes as a major proximal dust source for late Pleistocene loess in the Negev Desert, Israel , 2008, Quaternary Research.

[28]  Naomi Porat,et al.  Paleosols of the southern coastal plain of Israel , 2008 .

[29]  E. Garzanti,et al.  Petrology of Nile River sands (Ethiopia and Sudan): Sediment budgets and erosion patterns , 2006 .

[30]  A. Wintle,et al.  Thermally transferred luminescence in fine-grained quartz from Chinese loess : Basic observations , 2006 .

[31]  A. Murray,et al.  A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols , 2006 .

[32]  A. Murray,et al.  The single aliquot regenerative dose protocol: potential for improvements in reliability , 2003 .

[33]  A. Murray,et al.  Luminescence dating of quartz using an improved single aliquot regenerative-dose protocol , 2000 .

[34]  D. Gill,et al.  Marine Sand Resources Offshore Israel , 2000 .

[35]  N. Porat,et al.  Evolution of the Southeastern Mediterranean Coastal Plain , 2017 .

[36]  C. Mallol,et al.  Depositional and Paleoenvironmental setting of the Bizat Ruhama early pleistocene archaeological assemblages, Northern Negev, Israel: A microstratigraphic perspective , 2011 .

[37]  A. Murray,et al.  Luminescence dating of old (>70 ka) Chinese loess: A comparison of single-aliquot OSL and IRSL techniques , 2007 .

[38]  Naomi Porat,et al.  The middle to Late-Pleistocene sand sheet sequence of Kerem Shalom, western Negev - an archive of coastal sand incursion , 2007 .

[39]  S. Laukhin,et al.  New data on the Geology and Geochronology of the Lower Palaeolithic Site Bizat Ruhama in the Southern Levant , 2001 .

[40]  J. Feathers,et al.  An introduction to optical dating , 2000 .