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71.
Nicolas Hawie Remy Deschamps Fadi H. Nader Christian Gorini Carla Müller Delphine Desmares Ahmed Hoteit Didier Granjeon Lucien Montadert François Baudin 《Arabian Journal of Geosciences》2014,7(4):1323-1349
This paper presents an updated review of the Upper Mesozoic and Cenozoic sedimentological and stratigraphic evolution of the Levant margin with a focus on the northern Lebanon. Facies and microfacies analysis of outcrop sections and onshore well cores (i.e., Kousba and Chekka) supported by nannofossil and planktonic foraminifers biostratigraphy, allowed to constrain the depositional environments prevailing in the Turonian to Late Miocene. The “Senonian” (a historical term used to define the Coniacian to Maastrichtian) source rock interval was subdivided into four sub-units with related outer-shelfal facies: (1) Upper Santonian, (2) Lower, (3) Upper Campanian, and (4) Lower Maastrichtian. This Upper Cretaceous rock unit marks the major drowning of the former Turonian rudist platform. This paper confirms the Late Lutetian to Late Burdigalian hiatus, which appears to be a direct consequence of major geodynamic events affecting the Levant region (i.e., the continued collision of Afro-Arabia with Eurasia), potentially enhanced by regressional cycles (e.g., Rupelian lowstand). The distribution of Late Burdigalian–Serravallian rhodalgal banks identified in northern Lebanon was controlled by pre-existing structures inherited from the pulsating onshore deformation. Reef barriers facies occur around the Qalhat anticline, separating an eastern, restricted back-reef setting from a western, coastal to open marine one. The acme of Mount Lebanon’s uplift and exposure is dated back to the Middle–Late Miocene; it led to important erosion of carbonates that were subsequently deposited in paleo-topographic lows. The Late Cretaceous to Cenozoic facies variations and hiatuses show that the northern Lebanon was in a higher structural position compared to the south since at least the Late Cretaceous. 相似文献
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Nicolas Van Nieuwenhove Henning A. Bauch Frédérique Eynaud Evguenia Kandiano Elsa Cortijo Jean-Louis Turon 《Quaternary Science Reviews》2011,30(7-8):934-946
The Last Interglacial (Marine Isotopic Stage or MIS 5e) surface ocean heat flux from the Rockall Basin (NE Atlantic) towards the Arctic Ocean was reconstructed by analysing dinoflagellate cyst (dinocyst) assemblages in four sediment cores. Together with records of stable isotopes and ice-rafted detritus, the assemblage data reflect the northward retreat of ice(berg)-laden waters and the gradual development towards interglacial conditions at the transition from the Saalian deglaciation (Termination II) into MIS 5e. At the Rockall Basin, this onset of the Last Interglacial is soon followed by the appearance of the thermophilic dinocyst species Spiniferites mirabilis, with relative abundances higher than those observed at present in the area. North of the Iceland-Scotland Ridge, however, S. mirabilis only appears in significant numbers during late MIS 5e, between ~118 and 116.5 ka. Hence, fully marine Last Interglacial conditions with most intense Atlantic surface water influence occurred during late MIS 5e in the Nordic seas, and consequently also farther north in the Arctic Ocean, and at times when northern hemisphere summer insolation was already significantly decreased. The stratigraphic position of this Late Interglacial optimum is supported by planktic foraminifers and contrasts with the timing of the early Holocene climatic optimum in this area. We interpret the delayed northward expansion of Atlantic waters towards the polar latitudes as a result of the Saalian ice sheet deglaciation and its specific impact on the subsequent water mass evolution in this region. 相似文献
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Bachoc François Durrande Nicolas Rullière Didier Chevalier Clément 《Mathematical Geosciences》2022,54(5):941-977
Mathematical Geosciences - Kriging is a widely employed technique across computer experiments, machine learning and geostatistics. An important challenge for kriging is its high costs when dealing... 相似文献
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大数据对人文—经济地理学研究的促进与局限 总被引:15,自引:7,他引:8
大数据技术的诞生不仅快速推动着社会的进步,而且也将科学研究不断引向新的高度。以人类社会经济活动为主要研究对象的人文—经济地理学与当前大数据建设和发展趋势具有高度一致性,大数据的发展对丰富和完善人文—经济地理学势必起到积极的推动作用,同时也对人文—经济地理学的学科思维和研究方法提出了新的挑战。梳理和分析了目前大数据在人文—经济地理学主要研究领域,包括城市内部空间研究、交通与消费行为、社会空间与社会网络研究中的最近进展,以及大数据对参与式研究和决策平台的作用。着重剖析了大数据对人文—经济地理学数据获取,研究思维与范式,研究内容、研究时空尺度与研究目标等方面的促进作用与存在问题,特别是由于大数据自身发展的不完善,在数据收集特别是数据属性方面还存在很大的局限,缺乏理论基础将会使得大数据与实际应用受到很大限制,同时,数据本身也不能替代研究者思维和决策过程。因此,人文—经济地理学者应该科学对待大数据所带来的机遇,弥补和丰富以往发展中的短板,即完善学科数据建设、建立大数据应用较为完善的研究方法体系,促进跨域数据整合和跨域研究,以及推进研究对象和研究目的的转变。 相似文献
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