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首页> 外文期刊>Geodinamica Acta >Reply to discussion of ?Relative sea level fluctuations in Aegean coastal areas from middle to late Holocene? by Pavlopoulos [Geodinamica Acta 23/5-6 (2010) 225-232]
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Reply to discussion of ?Relative sea level fluctuations in Aegean coastal areas from middle to late Holocene? by Pavlopoulos [Geodinamica Acta 23/5-6 (2010) 225-232]

机译：答复有关“从中全新世到晚期的爱琴海沿岸地区相对海平面波动”的讨论作者：帕夫洛普洛斯[Geodinamica Acta 23 / 5-6（2010）225-232]

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This paper gives an answer to the criticism of Jussereta and Baeteman to the paper Discussion of "Relative sea level fluctuations in Aegean coastal areas from middle to late Holocene" by Kosmas Pavlopoulos [Geodinamica Acta 23/5-6 (2010) 225-232]. Jussereta and Baeteman were critical about how the peat beds can be regarded as certain sea level indicators. It is evident that the method adopted for the determination of the mean sedimentation rate of the peats beds is the dating of two distinct (usually basal and uppermost) layers. A common inaccuracy that some researchers do when they refer to relative sea level changes, is to focus only on eustatic component of this process, and to ignore the rest two (isostatic and tectonic). Jussereta and Baeteman do not believe that a particulate site could suffer alternate stages of subsidence and uplift. However, Aegean Sea is an area of high tectonic potential, which has shaped by the interplay compression and extension forces. Finally, this answer gives evidence that the observational data concerning the Holocene RSL stands in unstable localities can be compared with those data extracted from a hydro-isostatic model to estimate rates of vertical displacement and, therefore, to detect uplifting, relative stable and subsiding regions. This approach is followed by many researchers who study various Mediterranean coasts
机译：本文针对Jussereta和Baeteman对Kosmas Pavlopoulos撰写的“爱琴海沿海地区从全新世晚期到晚期全新世的相对海平面波动”的批评提供了答案[Geodinamica Acta 23 / 5-6（2010）225-232] 。 Jussereta和Baeteman对于如何将泥炭床视为某些海平面指示器至关重要。显然，确定泥炭床平均沉降速率所采用的方法是对两个不同的（通常是基底层和最上层）层进行测年。一些研究人员在谈到相对海平面变化时的一个普遍不准确之处是，只专注于这一过程的欣喜分量，而忽略了其余两个（等静和构造）。 Jussereta和Baeteman认为，一个微粒位置可能不会经历沉降和隆升的交替阶段。然而，爱琴海是一个构造潜力高的地区，它受到相互作用的压缩和伸展力的影响而形成。最后，这个答案提供了证据，可以将关于全新世RSL站在不稳定地区的观测数据与从水等静压模型中提取的数据进行比较，以估计垂直位移的速率，从而检测出隆起，相对稳定和下陷的区域。许多研究人员都采用这种方法来研究地中海沿岸

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