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Assessing regional geodiversity: the Iberian Peninsula

机译:评估区域地理多样性:伊比利亚半岛

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摘要

Geodiversity is a landscape characteristic related to the heterogeneity of the physical properties of the earth surface. in this work, we quantify and compare geodiversity in several geodynamic zones of the Iberian Peninsula. For this purpose, we have developed a geographic information system (GIS) procedure to carry out a regional terrain classification based on geodiversity factors. A classification process helped to produce a morphometric map (10 classes), a morphoclimatic map (five classes) and a geological map (15 classes). These three maps were combined using an overlay operation (union) to obtain the final terrain classification (419 classes), which was then applied to calculate diversity landscape indices. The latter were calculated using common landscape diversity indices (Patch Richness Density, Shannon's Diversity Index, Shannon's Evenness Index, Simpson's Diversity Index and Simpson's Evenness Index), provided by FRAGSTATS free software. These indices were calculated for the whole landscape of the main Iberian geological regions, thus revealing a close relationship between some index values and the geological and geomorphological characteristics. The highest diversity values are associated with Alpine collisional orogens and reactivated chains of the Precambrian-Palaeozoic massif. Intraplate orogen with sedimentary cover, characterized by extensive planation surfaces, have lower values. Mesozoic areas with no significant tectonic deformation and Cenozoic basins are characterized by the lowest diversity values. Amongst the latter, the major diversity is associated with the most dissected basins, which also present higher morphoclimatic variety. Though depending on the chosen scale and the landscape classification criteria, these indices provide an objective assessment of the regional geodiversity of Iberia.
机译:地球多样性是一种与地表物理特性异质性有关的景观特征。在这项工作中,我们量化并比较了伊比利亚半岛几个动力学区的地球多样性。为此,我们开发了一种地理信息系统(GIS)程序,以根据地理多样性因素进行区域地形分类。分类过程有助于生成形态计量图(10类),形态气候图(5类)和地质图(15类)。使用叠加操作(联合)将这三个地图组合在一起,以获得最终的地形分类(419类),然后将其应用于计算多样性景观指数。后者是使用FRAGSTATS免费软件提供的常见景观多样性指数(斑块密度,香农多样性指数,香农均匀度指数,辛普森多样性指数和辛普森均匀度指数)计算得出的。这些指数是针对伊比利亚主要地质区域的整体景观计算得出的,从而揭示了一些指数值与地质和地貌特征之间的密切关系。最高的多样性值与高寒碰撞造山带和前寒武纪-古生代地块的活化链有关。具有广泛覆盖的平坦表面特征的带沉积覆盖层的板内造山带的值较低。没有明显构造变形的中生代地区和新生代盆地具有最低的多样性值。在后者中,主要的多样性与解剖最多的盆地有关,这些盆地也表现出较高的形态气候多样性。尽管取决于所选择的规模和景观分类标准,但这些指数提供了对伊比利亚地区地理多样性的客观评估。

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