ebook img

Sedimentary Geology 1999: Vol 123 Table of Contents PDF

3 Pages·1999·0.4 MB·English
by  
Save to my drive
Quick download
Download
Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.

Preview Sedimentary Geology 1999: Vol 123 Table of Contents

Sedimentary Geology & ‘Ve u} ELSEVIER Sedimentary Geology 123 (1999) 277-278 Contents Volume 123, 1999 Research Papers Late Miocene Mediterranean desiccation: topography and significance of the ‘Salinity Crisis’ erosion surface on-land in southeast Spain i: : Dies, Fe, ND ksi aS eR Ree ee ek 2 Oo Oe ee Se ee Timing and genesis of early marine caymanites in the hydrothermal palaeokarst system of Buda Hills, Hungary ee ee. errr rere re rar er ee a Ce sr ree Sedimentology of the Cretaceous Maha Sarakham evaporites in the Khorat Plateau of northeastern Thailand ee Ss, %.. Sr PS GS ... I gk kw en eeewhe we ees Lower Ordovician iron ooids and associated oolitic clays in Russia and Estonia: a clue to the origin of iron oolites? 2, en, 7a: SU OE ea IE kk ks ee A ee ce ee ek Ew hg lw Ce ee a ce Progressive changes in sedimentary facies and stratal patterns along the strike-slip margin, northeastern Jinan Basin (Cretaceous), southwest Korea: implications for differential subsidence ek RI ns I og one wk 9 NW AO SOR Oe ee eS 8] Facies analysis and sequence stratigraphy of a Miocene warm-temperate carbonate ramp, Montagna della Maiella, Italy Pac en I I cos es Sn a ke ee A ee ee ee 103 Pore water evolution in sandstones of the Groundhog Coalfield, northern Bowser Basin, British Columbia ee nny NN a i pine oe ee ew OE CA a 6 es 129 Discussion Low limit of Mn?*-activated cathodoluminescence in calcite: state of the art — comment I ee og Oe ele cate eg Cee eigen IO Noe a tea Aaa ein ig. g-eses mS Wiw d we ae 147 Low limit of Mn**-activated cathodoluminescence of calcite: state of the art — reply ic), Pee 207 e. Pees OE, Cg ik kk ck ie bes ee oes ee eee we lee bbe ae ee ee 149 Kinematic indicators in fault gouge: tectonic analogy for soft-bedded ice sheets — comment ae On re ee yg ee ie Glued tig tg 2 alla igs ais Yop aee h Gee ee ae aR a)a 153 Kinematic indicators in fault gouge: tectonic analog for soft-bedded ice sheets — reply es ys ches aay a re tig is wigan ay: at a*d eie e aca span ew e-em hel wew ae gee 157 ExpresSed Hummocky moraine: sedimentary record of stagnant Laurentide Ice Sheet lobes resting on soft beds a, yg 48 ie ae ee we a WOK Wg KW Be ew ce Ke Wel ee Coe 163 Erosional remnants and pockets evolving from biotic—physical interactions in a Recent lower supratidal environ- ment 175 Research papers Facies architecture and sequence stratigraphy in glacially influenced basins: basic problems and water-level/ glacier input-point controls (with an example from the Quaternary of Ontario, Canada) ah a a sg? dcW we WK REO A Ne es I Se es ke 183 278 Contents Volume 123, 1999 Sedimentology of gravelly Lake Lahontan highstand shoreline deposits, Churchill Butte, Nevada, USA | 6S ee 199 ot Re 6 ES DR Se Se Re ee eS OE SD ee ee Se 8 eS OR SO ee, 8 ee eS OS Se SOS ES OS Se C6. Sedimentological characteristics and morphology of the aeolian sand dunes in the eastern part of the UAE, a case study from Ar Rub’ Al Khali Wad. BIORVOG 6.c5w e es 219 6.8 £288 S08 RS Oe ee Se Ree we ee OOD, Se AE SS SD ROS SRO Se ME ODO ESR SD UE OS Ae 4 SS A paleo-Brahmaputra? Subsurface lithofacies analysis of Miocene deltaic sediments in the Himalayan—Bengal system, Bangladesh A. Uddin and N. Lundberg 239 a, See ee ee ee A ee ee cae ee ee ee, SO A ee Se ee ee ee a ee a ee ee i i ee ee oe et a. oe oe ee er On ee a er ke The origin of sulphur in gypsum and dissolved sulphate in the Central Namib Desert, Namibia ED. Eckardt and B. Spiro . 255 he oe, ee a ee oe ee Me ae ee ee ee ee eet ee ee ee ee ee es ee a ee i ee ee oe oe oe ee 2, ce ae a, ce er oe a Author Index Volume 123, 1999 275 C56) eS 8 5e 6 ES OE: C8 2 AE Cee Ce ee ee SS Se Se AS eS BO PO OO Ee BES RS ew 8

See more

The list of books you might like

Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.