Awards presented by the International Association of Sedimentologists at the 19th International Sedimentological Congress,Geneva, Switzerland          下载免费PDF全文

Peir K. Pufahl 《Sedimentology》2015,62(4):1100-1101

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Tectonic control of accommodation space and sediment supply within the Mata Amarilla Formation (lower Upper Cretaceous) Patagonia,Argentina          下载免费PDF全文

Augusto N. Varela 《Sedimentology》2015,62(3):867-896

The Mata Amarilla Formation dates from the early Upper Cretaceous and was deposited during a transition in tectonic regime from the extensional Rocas Verdes Basin to the Austral Foreland Basin. Detailed sedimentological logs and architectural parameters were used to define 13 facies associations. The distribution of facies associations and associated variations in fluvial architecture have enabled large‐scale changes in accommodation space/sediment supply ratios (A/S ratio) to be defined for the three component sections of the Mata Amarilla Formation. The lower and upper sections are characterized by a high A/S ratio, whereas the middle section corresponds to a low A/S ratio. In the western part of the study area, small‐scale variations in the A/S ratio were recognized in the middle section. The strong west to east trend in evolution of the fluvial systems coincides with the direction of propagation of the Patagonian fold and thrust belt, which is located to the west of the study area. Intervals of high A/S ratio (i.e. lower and upper sections) are interpreted to have developed during periods of increased loading by the fold and thrust belt caused by tectonic uplift. In contrast, intervals of low A/S ratio (i.e. middle section) were developed during periods of tectonic quiescence. This article suggests that the large‐scale variations in A/S ratios are related to different rates of migration and growth of the Patagonian fold and thrust belt, whereas the small‐scale variation occurred in response to specific periods of thrusting and folding in the Patagonian fold and thrust belt (i.e. local loads). This field example of the effects of different scales of variation in A/S ratios across the Austral Foreland Basin could be used to recognize similar tectonically forced variations in stratigraphic architecture in other foreland basins throughout the world, as well as to understand the response of fluvial systems to such changes.  相似文献   

High‐resolution reconstruction of a coastal barrier system: impact of Holocene sea‐level change          下载免费PDF全文

Mikkel Fruergaard  Thorbjørn J. Andersen  Lars H. Nielsen  Peter N. Johannessen  Troels Aagaard  Morten Pejrup 《Sedimentology》2015,62(3):928-969

This study presents a detailed reconstruction of the sedimentary effects of Holocene sea‐level rise on a modern coastal barrier system. Increasing concern over the evolution of coastal barrier systems due to future accelerated rates of sea‐level rise calls for a better understanding of coastal barrier response to sea‐level changes. The complex evolution and sequence stratigraphic framework of the investigated coastal barrier system is reconstructed using facies analysis, high‐resolution optically stimulated luminescence and radiocarbon dating. During the formation of the coastal barrier system starting 8 to 7 ka rapid relative sea‐level rise outpaced sediment accumulation. Not before rates of relative sea‐level rise had decreased to ca 2 mm yr^?1 did sediment accumulation outpace sea‐level rise. From ca 5·5 ka, rates of regionally averaged sediment accumulation increased to 4·3 mm yr^?1 and the back‐barrier basin was filled in. This increase in sediment accumulation resulted from retreat of the barrier island and probably also due to formation of a tidal inlet close to the study area. Continued transgression and shoreface retreat created a distinct hiatus and wave ravinement surface in the seaward part of the coastal barrier system before the barrier shoreline stabilized between 5·0 ka and 4·5 ka. Back‐barrier shoreline erosion due to sediment starvation in the back‐barrier basin was pronounced from 4·5 to 2·5 ka but, in the last 2·5 kyr, barrier sedimentation has kept up with and outpaced sea‐level. In the last 0·4 kyr the coastal barrier system has been prograding episodically. Sediment accumulation shows considerable variation, with periods of rapid sediment deposition and periods of non‐deposition or erosion resulting in a highly punctuated sediment record. The study demonstrates how core‐based facies interpretations supported by a high‐resolution chronology and a well‐documented sea‐level history allow identification of depositional environments, erosion surfaces and hiatuses within a very homogeneous stratigraphy, and allow a detailed temporal reconstruction of a coastal barrier system in relation to sea‐level rise and sediment supply.  相似文献   

On the Proper Estimation of the Confidence Interval for the Design Formula of Blast-Induced Vibrations with Site Records   总被引：1，自引：0，他引：1  

W. M. Yan  Ka-Veng Yuen 《Rock Mechanics and Rock Engineering》2015,48(1):361-374

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Climatology and trends of summer high temperature days in India during 1969–2013     

JASWAL  A K  RAO  P C S  SINGH  VIRENDRA 《Journal of Earth System Science》2015,124(1):1-15

Journal of Earth System Science - Based on the daily maximum air temperature data from 176 stations in India from 1969 to 2013, the climatological distribution of the number of days with high...  相似文献   

Simulation of the Tornado Event of 22 March, 2013 over Brahmanbaria,Bangladesh using WRF Model with 3DVar DA techniques     

AHASAN  M N  ALAM  M M  DEBSARMA  S K 《Journal of Earth System Science》2015,124(1):37-48

Journal of Earth System Science - A severe thunderstorm produced a tornado (F2 on the enhanced Fujita–Pearson scale), which affected the Brahmanbaria district of Bangladesh during...  相似文献   

Simulation of iceberg drift as a component of ice monitoring in the West Arctic     

M. Yu. Kulakov  D. M. Demchev 《Russian Meteorology and Hydrology》2015,40(12):807-813

Discussed is the hydrodynamic model of iceberg drift. Presented are the examples ofits use in operational practice for predicting iceberg drift in the Kara Sea and for enhancing ice monitoring in the Barents Sea.  相似文献   

Seven-day intensity and intensity spread predictions for western North Pacific tropical cyclones     

Hsiao-Chung Tsai  Russell L. Elsberry 《Asia-Pacific Journal of Atmospheric Sciences》2015,51(4):331-342

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Performance of August–September Indian monsoon rainfall when June–July rainfall is reported as being in deficit/excess     

D. R. Kothawale  J. R. Kulkarni 《Meteorology and Atmospheric Physics》2015,127(2):147-161

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Variations of annual and seasonal runoff in Guangdong Province,south China: spatiotemporal patterns and possible causes   总被引：1，自引：0，他引：1  

Qiang Zhang  Mingzhong Xiao  Vijay P. Singh  Chong-Yu Xu  Jianfeng Li 《Meteorology and Atmospheric Physics》2015,127(3):273-288

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