印度尼西亚爪哇盆地东北部Rembang地区Selorejo组化石

Yody Rizkianto, Siti Umiyatun Choiriah, Achmad Subandrio, Intan Paramita Haty, Desi Kumala Isnani, Nanda Ajeng Nurwantari, Muhammad Ardiyan Syah Darmawa, Hendry Wirandoko
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引用次数: 0

摘要

东北爪哇盆地的Rembang地区是一个发展为石油系统的地区,是印度尼西亚石油储量最大的地区之一。其中一种岩性为碳酸化沉积岩,作为海相沉积的标志。露头连续,具丰富的微量化石,尤以勒德组和塞勒雷霍组最为突出。微量化石露头的存在对地球科学、生物学和其他科学的学习过程至关重要,但近年来这些露头已被封闭和破坏。由于社区采矿活动,它们的数量正在减少,因此必须立即对伦邦地区的痕迹化石进行独特的研究。本研究旨在发现在Selorejo组中发现的微量化石的变化。所使用的方法是野外测绘、测量地层测量、岩石取样和实验室分析(沉积学、岩石学和古生物学)。研究发现了Planolites、Helminthopsis、Thalassinoides、Conichnus、Chondrites、Macaronichnus、Bergauria、Ophiomorpha、Skolithos、Terebellina、Palaeophycus和Asterosoma的化石痕迹。
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Trace Fossils Of The Selorejo Formation, Rembang Zone, North East Java Basin, Indonesia
The Rembang Zone of the North East Java Basin is a zone that develops as a petroleum system and is one of the areas with Indonesia’s largest oil reserves. One of the lithologies in the Rembang Zone is a sedimentary rock carbonated as a marker of marine sediments. The outcrop is continuous and rich in trace fossils, especially in the Ledok and Selorejo Formations. The existence of trace fossil outcrops is crucial for the learning process of earth science, biology, and other sciences, but recently these outcrops have been closed and have become damaged. Their numbers are decreasing due to community mining activities, so unique research on trace fossils in the Rembang Zone must be done immediately. This research aims to discover the variation of trace fossils found in the Selorejo Formation. The methods used are field mapping, measured stratigraphic measurements, rock sampling, and laboratory analysis (sedimentology, petrography, and paleontology). The research shows trace fossils in Planolites, Helminthopsis, Thalassinoides, Conichnus, Chondrites, Macaronichnus, Bergauria, Ophiomorpha, Skolithos, Terebellina, Palaeophycus, and Asterosoma.
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