Rb–Sr geochronology of metamorphic rocks from the Central Indonesian Accretionary Collision Complex: Additional age constraints for the Meratus and Luk Ulo complexes (South Kalimantan and Central Java)

Alfing, Julian; Bröcker, Michael; Setiawan, Nugroho Imam

doi:10.1016/j.lithos.2021.105971

Cited by 8 publications

(1 citation statement)

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“…The creation of DOM using SfM will later be applied for other advanced analysis, such as aperture measurements on fractures within the scan window to be used as data for calculating the porosity prediction of basement fractures. Data collection will be carried out on metamorphic bedrock [4] outcrops that appear in the riverbed of Jurangjero Village, Sadangkulon District, Kebumen Regency, Central Java Province (Figure 1). [5].…”

Section: Introductionmentioning

confidence: 99%

Digital Fracture Porosity Measurement using Digital Outcrop Modelling (DOM)

Cahya Fardana,

Setianto,

Husein

2024

IOP Conf. Ser.: Earth Environ. Sci.

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Fracture measurements for porosity calculations often experience problems such as barely accessible locations, limited area coverage, and a long time to carry out field data measurements. Therefore, refined alternative methods are necessary to obtain the most favourable data. This study demonstrates fracture measurements through application of Digital Outcrop Modelling (DOM) using the Structure from Motion (SfM) method to utilize digital photogrammetry techniques. This method was chosen because data collection can be done remotely using Light Detection and Ranging (LiDAR) or digital photogrammetry to obtain point cloud data that is used to perform three-dimensional outcrop modeling. In addition, SfM also produces high-resolution data without the need for experts, is cost-efficient and safer than other methods. Hand-held platform Canon 700D digital single lens reflex (DSLR) camera was used in this study to capture data from an area of a square meter located on the riverbed that requires detailed modeling. DOM using SfM is applied to conduct aperture measurements in fractures inside the scan window, later used as data for calculating basement fracture porosity predictions. Field data collection is also carried out to validate data generated by DOM. Calculations achieved from field data and DOM data will be compared to determine differences of the porosity prediction values. Field data collection was carried out on 3 scan windows, each one is an area of 1 m2 and in totals obtained 117 fracture data, consist of 44 extension joints, 34 release joints, 7 shear joints, and 32 non-systematic joints. In this study, 115 photos were taken from scanwindow 1, 162 photos from scanwindow 2, and 158 photos from scanwindow 3 to construct the DOM using agisoft metashape software. The difference in these values can be used as a correction formula or evaluation for further research. The results of measuring basement fracture porosity using data generated by DOM will remain in the range of less than 1%.

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Section: Introductionmentioning

confidence: 99%

Digital Fracture Porosity Measurement using Digital Outcrop Modelling (DOM)

Cahya Fardana,

Setianto,

Husein

2024

IOP Conf. Ser.: Earth Environ. Sci.

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U–Pb zircon geochronology and geochemistry of Luk Ulo River boulders belong to Late Cretaceous-Paleocene metapsammite and metagranite of Luk Ulo Karangsambung, Central Java, Indonesia

Aminuddin

Shuaib

Akhtar

et al. 2023

Environ Sci Pollut Res

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The rock formation of late Cretaceous-Paleocene granite, metapsammite, and metagranite found across Luk Ulo Complex indicated boulders with diameter of approximately one meter and rounded shape along Luk Ulo River, Indonesia. However, less research found on geochronology and geochemistry has been conducted in study area, and such rocks require comprehensive understanding of magmatism and tectonic environment of Central Java, Indonesia. Therefore, the main objective of this study is to address the geochronological and geochemical age histories across Central Java, Indonesia using U-Pb zircon dating technique. Generally, most common types of rocks were observed which composed of hornblende and garnet-bearing granite, metapsammite, and metagranite. The geochemical study showed that protolith of rocks with hornblende was identi ed as Cordilleran granitoid (I-type), which originated from magmatic arc with basaltic differentiation. Further, protolith of rocks containing garnet was categorized as Caledonian granitoid (S-type), which is caused by post-collisional orogeny. The cluster observations of magmatic zircons reveal their magmatic ages, which vary from 67.00 + 1.2 to 69.10 + 0.91 Ma (late Cretaceous), whereas ages of inherited zircons ranged from 100 + 5 to 437 + 13 Ma (early Cretaceous to Silurian). Estimated periods of partial melting were found between 100-5 Ma and 118-4 Ma (early Cretaceous). Comparing the zircon ages of Luk Ulo with the zircon ages from the Sundaland regions reveals that the age distribution patterns are incredibly similar; the peak ages dispersed between the Cretaceous and Triassic periods, as well as Sundaland region was the source of the materials.

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