Tectonic-geomorphological map of the middle Aterno River valley (Abruzzo, Central Italy)

被引:32
|
作者
Santo, Antonio [1 ]
Ascione, Alessandra [2 ]
Di Crescenzo, Giuseppe [1 ]
Miccadei, Enrico [3 ]
Piacentini, Tommaso [3 ]
Valente, Ettore [2 ]
机构
[1] Univ Naples Federico II, Dept Civil Construct & Environm Engn DICEA, I-80125 Naples, Italy
[2] Univ Naples Federico II, Dept Earth Sci Environm & Georesources DiSTAR, I-80138 Naples, Italy
[3] G DAnnunzio Univ Chieti Pescara, Dept Engn & Geol INGEO, Lab Tecton Geomorphol & GIS, I-66100 Chieti, Italy
来源
JOURNAL OF MAPS | 2014年 / 10卷 / 03期
关键词
Italy; L'Aquila; intermontane tectonic basins; central apennines; tectonic geomorphology; EARTHQUAKE CENTRAL APENNINES; M-W; 6.3; LAQUILA EARTHQUAKE; SOUTHERN APENNINES; BASIN; FAULT; SANGRO; AREA; INSIGHTS; HISTORY;
D O I
10.1080/17445647.2013.867545
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
After the 6 April, 2009 normal faulting L'Aquila earthquake (Mw 6.3), the attention of many scientists was drawn to the Abruzzo Apennines. Until that time few studies had addressed the geomorphological and morphotectonic features of this area and none to extensive geomorphological mapping. The tectonic-geomorphological map (scale 1:40,000) presented in this work is the result of a morphotectonic investigation of the middle Aterno River valley, which includes the area from the western L'Aquila-Coppito basin (to the northwest) to the Paganica-San Demetrio basin and to the Castelnuovo-Civitaretenga basin (to the southeast). The map is implemented within a GIS environment by means of: DEM and map-based cartographic analysis and morphometry of orography and hydrography (raster and vector data scale 1:25,000, 10 m grid DEM), photogeological analysis (scale 1:10,000), structural geomorphological field mapping (scale 1:10,000), basin fill geometry analysis (geophysical and borehole investigations) and tectonic-geomorphological profiles that couple landforms, deposits and surfaces. The map incorporates orography and hydrography, basin fill geometry, tectonic-geomorphology and tectonic-geomorphological profiles. The result provides a basis for the recognition of morphotectonic features at basin scale, detection of tectonic control on the landscape, and reconstruction of paleo-landscapes and basin geometry.
引用
收藏
页码:365 / 378
页数:14
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