Chronology of Early to Mid-Pleistocene sediments in the northern North Sea: New evidence from amino acid and strontium isotope analyses     

《Quaternary Geochronology》2022

Sediments deposited during glacial-interglacial cycles through the Early to Mid-Pleistocene in the North Sea are chronologically poorly constrained. To contribute to the chronology of these units, amino acid racemization (AAR) and strontium (Sr) isotope analyses have been performed on samples from four shallow borings and one oil well along a transect in the northern North Sea. D/L Asp (aspartic acid) values obtained through reverse-phase liquid chromatography in the benthic foraminiferal species Elphidium excavatum is focused on because of consistent results and a good stratigraphic distribution of this benthic species. For the Early Pleistocene, an age model for the well 16/1–8, from the central part of the northern North Sea based on Sr ages allows for dating of the prograding wedges filling the pre-Quaternary central basin. A regional calibration curve for the racemization of Asp in Elphidium excavatum is developed using published ages of radiocarbon-dated samples and samples associated with the previously identified Bruhnes/Matuyama (B/M) paleomagnetic boundary and a Sr age from this study. Based on all the available geochronological evidence, samples were assigned to marine oxygen isotope stages (MIS) with uncertainties on the order of 10–70 ka.Sr ages suggest a hiatus of <2 million years (Ma) possibly due to non-deposition or low sedimentation between the Utsira Formation (Pliocene) and the Early Pleistocene. An increase in sedimentation rates around 1.5 ± 0.07 Ma (∼MIS 51) may partly be due to sediment supply from rivers from the south-east and partly due to the extension of ice sheet around 1.36 ± 0.07 Ma from the Norwegian coast to the central North Sea. A possible basin-wide glaciation occurred around 1.1 Ma (∼ MIS 32) (upper regional unconformity/top of unit Q4 in this study), resulting in erosion and regional unconformity. Two interglacials in the Norwegian Channel have been dated: the Radøy Interglacial to 1.07 ± 0.01 Ma (possibly MIS 31, the ‘super interglacial’), and the Norwegian Trench Interglacial to 0.50 ± 0.02 Ma (possibly MIS 13). A massive till unit identified at the same stratigraphic level in all shallow borings may partly represent an extensive MIS 12 glaciation. This study shows that the combined use of amino acid racemization data and Sr isotope chronology can refine the chronological ambiguities of Quaternary North Sea sediments related partly to the impact of glacial processes.  相似文献   

俯冲、碰撞、深断裂和埃达克岩与斑岩铜矿   总被引：32，自引：2，他引：30  

芮宗瑶  侯增谦  李光明  张立生  王龙生  唐索寒 《地质与勘探》2006,42(1):1-6

无论是碰撞前的B型俯冲,还是碰撞后的A型俯冲,形成斑岩铜矿都必须要有洋壳或上地幔为主的物质参与.因此斑岩铜矿的初始锶值都小于0.708,超过0.708,则意味地壳物质的增多,将形成斑岩钼矿和斑岩钨锡矿.斑岩铜矿带常常与切穿地壳的深断裂带平行共生,并产于其上盘,在该地带往往发育壳幔混合以幔为主的深源花岗质浅成-超浅成小斑岩体.含铜斑岩和埃达克岩可能均为俯冲和交代产物,因而具有相似的特征,但到俯冲末期它们分道扬镳了.文章通过对冈底斯斑岩铜(钼、金和多金属)矿带的分析,来讨论俯冲、碰撞和深断裂带与斑岩铜矿的关系.同时也通过我国中央碰撞造山带仅发育斑岩钼矿,而缺乏斑岩铜矿,从而证明上地幔物质的加入对斑岩铜(金)矿的重要意义.  相似文献   

CBERS-02B卫星WFI成像在轨MTF估算与图像MTF补偿   总被引：3，自引：2，他引：1       下载免费PDF全文

李小英  顾行发  余涛  程天海  高海亮  李家国  杨晓峰 《遥感学报》2009,13(3):377-390

基于高分辨率图像对比法, 利用同一卫星平台上空间分辨率19.5m的CCD相机图像对CBERS-02B卫星上空间分辨率为258m的 WFI成像仪图像进行在轨MTF(modulate transfer function)测量, 获得WFI(wide field imager)相机沿轨、跨轨与45o方向的MTF曲线, 并计算出3个方向的线扩展函数LSF(line spread function), 获得3个方向的有效半带宽。结果表明WFI相机红波段跨轨、沿轨与45o方向的有效半带宽, 即有效瞬时视场, 分别为1.188, 1.165与1.281个像元, 近红外波段为1.258, 1.195与1.326个像元。基于获得的MTF, 利用维纳滤波法对WFI图像进行补偿, 部分恢复了WFI图像的细部信息。  相似文献