地质Dimito区和Boalemo首都戈伦塔洛省周围

Alifia Widya Warapsari Badaru, Fitryane Lihawa, Intan Noviantari Manyoe
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引用次数: 1

摘要

在行政方面,研究区域涵盖两个区,沃诺萨里街道和戈伦塔洛省博阿莱莫区杜鲁皮街道。根据Gorontalo地区的地貌,研究区域位于Bone Tilamuta Modello的南部山区,通常由Gorontolo始新世-渐新世的古火山沉积岩层组成。本次地质研究的目的是发现Dimito及其周边地区形成的地质秩序,包括地貌、地层学、地质结构和地质历史等多个方面。研究结果表明,研究区的地貌分为三个地貌单元,即冲积平原、火山丘和剥蚀丘。研究区地层从中新世早期到全新世分为五类单元,即熔岩玄武岩Dimito(始新世早期)、Wackestone Dimito(始新世早期)、Andesit Kalidingin(中新世中期)、Granodiorite Bualo(上新世中期)和冲积Buaolo(Recen)。研究区所在地的地质构造相对呈东北-西南向西北-东南走向。从数据处理来看,研究区所在地的断层由正常左滑断层Kalidingin和滞后左滑断层Bualo组成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geologi Daerah Dimito dan Sekitarnya Kabupaten Boalemo Provinsi Gorontalo
Administratively, the research area covers two districts, Wonosari Sub-district and Dulupi Sub-district, Boalemo District, Gorontalo Province. Based on the physiography of the Gorontalo region, the research area which is included in the southern mountain zone of Bone-Tilamuta-Modello generally consists of ancient volcano-sedimentary rock formations in Gorontalo, the Eocene-Oligocene. The purpose of this geological research is to discover the geological order that developed in the area of Dimito and surrounding are as covering several aspect such as geomorphology, stratigraphy, geological structure, and geological history. The result shows that the geomorphology of the research area divided into three geomorphic units, namely the units of the Alluvial Plain, Volcanic Hills, and Denudasional Hills. Stratigraphy of the research area divided into five types of units sorted from the early Miocene to the Holocene, i.e., Lava Basal Dimito (Early Eocene), Wackestone Dimito (Early Eocene), Andesit Kalidingin (Middle Miocene), Granodiorite Bualo (Middle Pliocene), and Alluvial Buaolo (Recen). Geological structures that work on the location of the research area relatively trend from northeast-southwest to northwest-southeast. Fault working on the location of the research area from the data processing consists of Normal Left Slip Fault Kalidingin and Lag Left Slip Fault Bualo.
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