Controls on sand ramp formation in southern Namibia
暂无分享,去创建一个
[1] P. Srivastava,et al. Late Pleistocene aeolian activity in the cold desert of Ladakh: A record from sand ramps , 2017 .
[2] Lluís Gómez-Pujol,et al. Middle to Late Pleistocene dunefields in rocky coast settings at Cala Xuclar (Eivissa, Western Mediterranean): Recognition, architecture and luminescence chronology , 2016 .
[3] P. Reimer,et al. 50,000-years of vegetation and climate change in the southern Namib Desert, Pella, South Africa , 2016 .
[4] G. Duller,et al. DRAC: Dose Rate and Age Calculator for trapped charge dating , 2015 .
[5] L. Mcfadden,et al. Impacts of climate change on the formation and stability of late Quaternary sand sheets and falling dunes, Black Mesa region, southern Colorado Plateau, USA , 2015 .
[6] A. Mather,et al. Extensive Quaternary aeolian deposits in the Drakensberg foothills, Rooiberge, South Africa , 2014 .
[7] K. Heine,et al. Several distinct wet periods since 420 ka in the Namib Desert inferred from U-series dates of speleothems , 2014, Quaternary Research.
[8] N. Mountney,et al. Remote sensing of spatial variability in aeolian dune and interdune morphology in the Rub’ Al-Khali, Saudi Arabia , 2013 .
[9] A. Stone. Age and dynamics of the Namib Sand Sea: A review of chronological evidence and possible landscape development models , 2013 .
[10] A. Goudie. Arid and Semi-Arid Geomorphology , 2013 .
[11] G. Guérin,et al. On the use of the infinite matrix assumption and associated concepts: A critical review , 2012 .
[12] Dr Robert Bryant,et al. On the formation of sand ramps: A case study from the Mojave Desert , 2012 .
[13] P. Vermeesch,et al. Petrology of the Namib Sand Sea: Long-distance transport and compositional variability in the wind-displaced Orange Delta , 2012 .
[14] Z. Dong,et al. Airflow patterns upwind of obstacles and their significance for echo dune formation: A field measurement of the effects of the windward slope angle , 2012, Science China Earth Sciences.
[15] David S. G. Thomas,et al. Interpreting geoproxies of late Quaternary climate change in African drylands: Implications for understanding environmental change and early human behaviour , 2012 .
[16] Z. Dong,et al. Mean airflow patterns upwind of topographic obstacles and their implications for the formation of echo dunes: A wind tunnel simulation of the effects of windward slope , 2011 .
[17] G. Duller,et al. The fast ratio: A rapid measure for testing the dominance of the fast component in the initial OSL signal from quartz , 2011 .
[18] B. Schütt,et al. Geoarcheology and Chronostratigraphy in the Vicinity of Meroitic Naga in Northern Sudan - a Review , 2011 .
[19] M. Blair,et al. Thermal history versus sedimentary history: OSL sensitivity of quartz grains extracted from rocks and sediments , 2011 .
[20] H. Viles,et al. Can 234U–230Th dating be used to date large semi‐arid tufas? Challenges from a study in the Naukluft Mountains, Namibia , 2010 .
[21] Dr Robert Bryant,et al. The Namib Sand Sea digital database of aeolian dunes and key forcing variables , 2010 .
[22] M. Meadows,et al. Evidence for progressive Holocene aridification in southern Africa recorded in Namibian hyrax middens: Implications for African Monsoon dynamics and the ‘‘African Humid Period’’ , 2010, Quaternary Research.
[23] Timothy T. Barrows,et al. OSL dating of southeast Australian quartz: A preliminary assessment of luminescence characteristics and behaviour , 2010 .
[24] J. Moersch,et al. Climbing and falling dunes in Valles Marineris, Mars , 2010 .
[25] David S. G. Thomas,et al. Late Quaternary palaeohydrological changes in the northern Namib Sand Sea: New chronologies using OSL dating of interdigitated aeolian and water-lain interdune deposits , 2010 .
[26] M. Meadows,et al. A record of rapid Holocene climate change preserved in hyrax middens from southwestern Africa , 2009 .
[27] Z. Dong,et al. Geomorphological hierarchies for complex mega-dunes and their implications for mega-dune evolution in the Badain Jaran Desert , 2009 .
[28] B. Chase. Evaluating the use of dune sediments as a proxy for palaeo-aridity: A southern African case study , 2009 .
[29] T. Pietsch,et al. Fluvial transport as a natural luminescence sensitiser of quartz , 2008 .
[30] G. Duller. Single‐grain optical dating of Quaternary sediments: why aliquot size matters in luminescence dating , 2008 .
[31] David S. G. Thomas,et al. Linear dune accumulation chronologies from the southwest Kalahari, Namibia: challenges of reconstructing late Quaternary palaeoenvironments from aeolian landforms , 2008 .
[32] David S. G. Thomas,et al. Late Quaternary linear dune accumulation and chronostratigraphy of the southwestern Kalahari: implications for aeolian palaeoclimatic reconstructions and predictions of future dynamics , 2007 .
[33] M. Meadows,et al. Late Quaternary dynamics of southern Africa's winter rainfall zone , 2007 .
[34] Nicholas Lancaster,et al. Age and dynamics of linear dunes in the Namib Desert , 2007 .
[35] U. Schreiber,et al. Mesoproterozoic rocks of Namibia and their plate tectonic setting , 2006 .
[36] A. Murray,et al. Stability of the quartz fast-component in insensitive samples , 2006 .
[37] Larry W. Lake,et al. Pattern analysis of dune‐field parameters , 2006 .
[38] A. Murray,et al. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols , 2006 .
[39] N. Lancaster,et al. Combining ground penetrating radar surveys and optical dating to determine dune migration in Namibia , 2005, Journal of the Geological Society.
[40] R. Bailey,et al. The measured dependence of laboratory beta dose rates on sample grain size , 2005 .
[41] Tao Wang,et al. Geomorphology of the megadunes in the Badain Jaran Desert , 2004 .
[42] A. Murray,et al. Developments in radiation, stimulation and observation facilities in luminescence measurements , 2003 .
[43] G. Duller. Distinguishing quartz and feldspar in single grain luminescence measurements , 2003 .
[44] I. Makhlouf,et al. Recent colluvial sedimentation in Jordan: fans evolving into sand ramps , 2002 .
[45] N. Lancaster. How dry was dry?-Late Pleistocene palaeoclimates in the Namib Desert , 2002 .
[46] K. Pye,et al. GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments , 2001 .
[47] Sharon E. Nicholson,et al. The nature of rainfall variability over Africa on time scales of decades to millenia , 2000 .
[48] A. Murray,et al. Luminescence sensitivity changes in natural quartz induced by high temperature annealing: a high frequency EPR and OSL study , 2000 .
[49] G. Laslett,et al. OPTICAL DATING OF SINGLE AND MULTIPLE GRAINS OF QUARTZ FROM JINMIUM ROCK SHELTER, NORTHERN AUSTRALIA: PART I, EXPERIMENTAL DESIGN AND STATISTICAL MODELS* , 1999 .
[50] L. Sen,et al. Wind tunnel simulation experiment of mountain dunes , 1999 .
[51] Andrew C. Morton,et al. Processes controlling the composition of heavy mineral assemblages in sandstones , 1999 .
[52] A. Warren,et al. The palaeoenvironmental significance of dune size hierarchies , 1998 .
[53] A. Rodríguez‐Perea,et al. Morphology and architecture of a late Pleistocene cliff‐front dune, Mallorca, Western Mediterranean , 1997 .
[54] S. O'Hara,et al. Development and Environmental Significance of an Eolian Sand Ramp of Last-Glacial Age, Central Iran , 1997, Quaternary Research.
[55] H. Rendell,et al. Luminescence dating of sand ramps in the Eastern Mojave Desert , 1996 .
[56] N. Lancaster,et al. Geomorphology and sediments of sand ramps in the Mojave desert , 1996 .
[57] S. McKeever,et al. Luminescence sensitivity changes in quartz as a result of annealing , 1995 .
[58] J. Prescott,et al. Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations , 1994 .
[59] N. Lancaster. The development of large aeolian bedforms , 1988 .
[60] N. Lancaster. Winds and sand movements in the Namib Sand Sea , 1985 .
[61] M. Seely,et al. Local winds over the central Namib. , 1980 .
[62] F. Netterberg. The Interpretation of Some Basic Calcrete Types , 1969 .
[63] R. Folk,et al. Brazos River bar [Texas]; a study in the significance of grain size parameters , 1957 .
[64] G. W. Lamplugh. ‘Calcrete.’ , 1902, Geological Magazine.
[65] A. Ioannides,et al. A RE-EVALUATION OF RADIATION DOSE-RATE CONVERSION FACTORS , 2014 .
[66] R. Neumann,et al. Cinnamaldehyde in early iron age phoenician flasks raises the possibility of levantine trade with South East Asia , 2013 .
[67] M. Telfer,et al. Sand ramps in the Golden Gate Highlands National Park, South Africa: Evidence of periglacial aeolian activity during the last glacial , 2012 .
[68] A. Sawakuchi,et al. Correlation between thermoluminescence sensitivity and crystallization temperatures of quartz: Potential application in geothermometry , 2011 .
[69] Pierrick Gaudry,et al. Point Counting , 2011, Encyclopedia of Cryptography and Security.
[70] Heng Tao Shen,et al. Principal Component Analysis , 2009, Encyclopedia of Biometrics.
[71] N. Lancaster. Dune Morphology and Dynamics , 2009 .
[72] Bertram Silke. Late Quaternary sand ramps in south-western Namibia , 2003 .
[73] V. P. Tchakerian,et al. Geochemistry of sediments from Quaternary sand ramps in the southeastern Mojave Desert, California , 2003 .
[74] André F. Lotter,et al. Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results , 2001 .
[75] N R J Poolton,et al. Luminescence sensitivity changes in natural quartz induced by high temperature annealing: a high frequency EPR and OSL study , 2000 .
[76] Kenneth Pye,et al. Aeolian sand and sand dunes , 1990 .
[77] Lancaster,et al. Climate of the central Namib Desert , 1984 .
[78] H. Tsoar. Wind Tunnel Modeling of Echo and Climbing Dunes , 1983 .