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首页> 外文期刊>Marine Geology >Reply to the comment on 'Late Quaternary depositional history of the North Evvoikos Gulf, Aegean Sea, Greece' Marine Geology, 232, 157-172, 2006
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Reply to the comment on 'Late Quaternary depositional history of the North Evvoikos Gulf, Aegean Sea, Greece' Marine Geology, 232, 157-172, 2006

机译：对“希腊爱琴海北部Evvoikos海湾晚第四纪沉积历史”的评论的答复，海洋地质，232，157-172，2006年

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摘要

We reply here to comments of Stiros and Pirazzoli (Marine Geology, 2007) who suggest that the rates of global sea-level fluctuation and their amplitudes are only parts of a complex of forces, in particular tectonics and volcanism. Those forces according to their model shaped and changed the morphology and history of most marine areas around Greece. They apply this model to our study area, the Northern Evvoikos Gulf, as well as to some areas elsewhere. For the Evvoikos Gulf as well as many other marine areas of the Aegean and Ionian Seas (see Perissoratis and Mitropoulos, 1989; Piper and Perissoratis, 1991; Perissoratis and van Andel, 1991; van Andel et al., 1993), we have assembled and published a large marine data base. In particular in a paper by Perissoratis and Conispoliatis (2003) the data we collected show beyond any reasonable doubt that the major force controlling the late Quaternary depositional history and shape of the sea-floor around Greece were formed by global sea-level changes driven by the numerous glaciation-interglacial cycles of the Pleistocene. In that paper we studied about 20 regions of the Aegean and Ionian Seas including the North and South Ewoikos Gulfs in great detail, also taking into account the sedimentary record, all seismic reflection data, tectonism and even some geo-archaeological evidence, but the force that shaped the history and morphology of each area again was without question the work of the repeated cycles of Pleistocene sea-level changes.
机译：我们在此答复Stiros和Pirazzoli的评论（海洋地质，2007年），他们认为全球海平面涨落的速度及其振幅只是复杂力量的一部分，尤其是构造学和火山作用。这些部队根据他们的模型塑造并改变了希腊周围大多数海域的形态和历史。他们将此模型应用于我们的研究区域，北部Evvoikos海湾以及其他地区。对于Evvoikos海湾以及爱琴海和爱奥尼亚海的许多其他海域（请参见Perissoratis和Mitropoulos，1989; Piper和Perissoratis，1991; Perissoratis和van Andel，1991; van Andel等，1993）。并发布了一个大型海洋数据库。特别是在Perissoratis和Conispoliatis（2003）的一篇论文中，我们收集的数据毫无疑问地表明，控制后期第四纪沉积历史和希腊周围海底形态的主要力量是由全球海平面变化驱动的。更新世的众多冰河间期循环。在那篇论文中，我们详细研究了爱琴海和爱奥尼亚海的20个区域，包括北部和南部的Ewoikos海湾，还考虑了沉积记录，所有地震反射数据，构造论甚至一些地质考古证据，但是毫无疑问，再次塑造每个地区的历史和形态的是更新世海平面变化重复周期的工作。

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