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Morphostructure Analysis of Sapaya Ancient Volcanic Area Based Lineament Data

机译:基于Sapaya古代火山地区的语气结构分析

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Morphostructure of Sapaya ancient volcanic have been analysis by using lineament models. In this models, two methods of retrieval data have been used. First, the field survey of the area, second, the satellite images analysis. The morphostructure of Sapaya ancient volcanic contribute to the crater, caldera, and shown an eroded cone morphology. The directions of eruption from Sapaya ancient volcanic have identified in region of Jeneponto and Takalar, which is had east - west and northeast - southwest structure. These eruptions also give contribution to the character of river in Jenelata watershed, by the presence of tuffs, pillow lava, basalt, andesite, diorite, granodiorite, granite, and gabbro, respectively.
机译:Sapaya古老的火山的形态学已经通过使用谱系模型进行了分析。 在此模型中,已使用两种检索数据。 首先,该地区的实地调查,第二,卫星图像分析。 Sapaya古代火山的形态学促成了火山口,卡尔德岛,并显示出一种侵蚀的锥体形态。 Sapaya古代火山爆发的爆发方向在Jeneponto和Takalar的地区确定,该地区已成为东部和东北 - 西南结构。 这些爆发还通过凝灰岩,枕头熔岩,玄武岩,安德莱特,Diority,Granodiorite,Granite和Gabbro来为Jenelata流域的河流的特征提供贡献。

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