{"title":"PETROGENESA BATUAN DIORIT PADA FORMASI DIORIT LEMBAI DESASNAIMBOY, KECAMATAN WARMARE, KABUPATEN MANOKWARI, PROVINSI PAPUA BARAT","authors":"Philipus Samuel","doi":"10.34151/technoscientia.v15i2.4262","DOIUrl":null,"url":null,"abstract":"Desa Snaimboy and it’s surroundings are a neolithic rock composed of diorite and localized gabbro (Pieters et al., 1990; Webb et al., 2020), which are widespread and form small mounds to the mountains. It is dominated by Tertiary intrusive igneous rocks. The purpose of this study is to analyze the characteristics and petrogenesis of diorite rocks in the Lembai Diorite Formation in the study area. Analysis that can describe the characteristics of lithology and the origin of rock formation is by carrying out petrological analysis and petrographic analysis. \nThe results of the petrological analysis show that the diorite in the Lembai Diorite Formation has a characteristic weathered color of brownish black and fresh black color with white spots. Granularity in general is faneric – porphyritic, euhedral – subhedral crystal form, holocrystalline – hypocrystalline crystallinity, with coarse – very coarse crystal size, and inequigranular crystal uniformity. The structure is generally massive. The mineral composition of diorite is composed of 5-10% quartz, 50-60% plagioclase, 10-20% k-feldspar, 30-40% hornblend, 1-3% biotite, 10-20% pyroxene (Travis, 1975). \nThe results of petrographic analysis show that the diorite in the Lembai Diorite Formation mainly consists of syenogranite and monzogranite. The type of magma formation is peraluminous or MPG (Muscovit-bearing Peraluminous Granite) type (Barbarin, 1999).","PeriodicalId":301828,"journal":{"name":"JURNAL TEKNOLOGI TECHNOSCIENTIA","volume":"19 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"JURNAL TEKNOLOGI TECHNOSCIENTIA","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.34151/technoscientia.v15i2.4262","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Desa Snaimboy and it’s surroundings are a neolithic rock composed of diorite and localized gabbro (Pieters et al., 1990; Webb et al., 2020), which are widespread and form small mounds to the mountains. It is dominated by Tertiary intrusive igneous rocks. The purpose of this study is to analyze the characteristics and petrogenesis of diorite rocks in the Lembai Diorite Formation in the study area. Analysis that can describe the characteristics of lithology and the origin of rock formation is by carrying out petrological analysis and petrographic analysis.
The results of the petrological analysis show that the diorite in the Lembai Diorite Formation has a characteristic weathered color of brownish black and fresh black color with white spots. Granularity in general is faneric – porphyritic, euhedral – subhedral crystal form, holocrystalline – hypocrystalline crystallinity, with coarse – very coarse crystal size, and inequigranular crystal uniformity. The structure is generally massive. The mineral composition of diorite is composed of 5-10% quartz, 50-60% plagioclase, 10-20% k-feldspar, 30-40% hornblend, 1-3% biotite, 10-20% pyroxene (Travis, 1975).
The results of petrographic analysis show that the diorite in the Lembai Diorite Formation mainly consists of syenogranite and monzogranite. The type of magma formation is peraluminous or MPG (Muscovit-bearing Peraluminous Granite) type (Barbarin, 1999).
Desa Snaimboy及其周围是由闪长岩和局部辉长岩组成的新石器时代岩石(Pieters et al., 1990;Webb et al., 2020),它们分布广泛,在山上形成小土丘。以第三系侵入火成岩为主。本研究的目的是分析研究区伦白闪长岩组闪长岩的特征及其成因。通过岩石学分析和岩相学分析,可以描述岩性特征和岩层成因。岩石学分析结果表明,伦白闪长岩组闪长岩具有棕黑、鲜黑带白斑的风化色特征。粒度一般为双晶-斑状,自面体-亚面体晶型,全晶-次晶型,晶粒尺寸粗-极粗,晶粒均匀性不均匀。结构通常是巨大的。闪长岩矿物组成为石英5-10%、斜长石50-60%、钾长石10-20%、角长石30-40%、黑云母1-3%、辉石10-20% (Travis, 1975)。岩石学分析结果表明,伦白闪长岩组闪长岩主要由正长花岗岩和二长花岗岩组成。岩浆形成类型为过铝质或MPG(含muscovita过铝质花岗岩)型(Barbarin, 1999)。