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Engineering-geological investigation and risk assessment for disaster management in the Purworejo Regency, Central Java, Indonesia

机译:印度尼西亚中部爪哇省武力堂灾区灾害管理的工程 - 地质调查与风险评估

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In the Purworejo regency, Central Java, there is a mountainous area, called Menoreh Hills. It is known as a disaster prone, tectonically representing volcanic arcs of the central part of Java Island of the tertiary era. The stratigraphy of the area varieties from the oldest to the youngest rocks, respectively consists of volcanic rocks of the Kaligesing and Dukuh formations, limestones of the Jonggrangan Formation, marl-calcarenite intermittent of Sentolo Formation, and alluvial deposits. The Kaligesing Formation consists of andesite pyroclastic breccia, tuffaceous breccia, and lava breccia, the Dukuh Formation consists of laharic breccia, Jonggrangan Formation comprises reef limestones, Sentolo Formation comprises layered calcarenite limestone, alternating with marl, while alluvial deposits include loose materials with various grain size. The geological structure found in the Menoreh Hills is in the form of joints and lateral slip faults with a general pattern of North West - Southeast and Northeast - Southwest. Especially the volcanic rocks in the Menoreh Hills have experienced extensive weathering, firming soil with a thickness reaches up to 5 meters. Because of the topography with a quite steep slope (>20° or >36%), the soil of quite thick (>2m), the presence of fracture structures that quite tight, triggered by high rainfall (.2000mm/year), Menoreh Hills can be classified as landslide prone areas. In connection with this, a risk assessment needs to be carried out in the context of developing disaster management in the Purworejo Regency area.
机译:在Purworejo Regency,中爪哇省,有一个山区,叫Menoreh Hills。它被称为易受灾害,构造了代表第三纪元的Java岛的中央部分的火山弧。从最古老的岩石到最古老的岩石的地区品种的地层分别由kaligesing和dukuh地层的火山岩组成,Jonggrangan的石灰岩,Marl-calcarenite的Sentolo形成和冲积沉积物。 kaligesing形成由安德莱氏菌,牙垢Breccia和Lava Breccia组成,Dukuh形成包括骆驼Breccia,Jonggrangan Freccia包括Reef Limestones,Sentolo形成包含分层的Calcarenite石灰石,与Marl交替,而冲积沉积物包括各种谷物的松散材料尺寸。 Menoreh Hills中发现的地质结构是关节和横向滑倒的形式,与西北和东北部的一般图案 - 西南部。特别是Menoreh Hills中的火山岩经历了广泛的风化,厚度的紧致土壤达到5米。由于具有相当陡坡(> 20°或> 36%)的地形,相当厚(> 2m)的土壤,骨折结构的存在非常紧张,由高降雨引发(.2000mm /年),menoreh山丘可以被归类为滑坡易发的地区。有关这一点,需要在普沃尔沃河丽晶地区的灾害管理方面进行风险评估。

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