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All Journal Forum Geografi Journal of Geoscience, Engineering, Environment, and Technology Jurnal Geosains dan Teknologi KURVATEK
Hita Pandita, Hita
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Civil Engineering, Building, Construction & Architecture Earth & Planetary Sciences Electrical & Electronics Engineering Energy Engineering Environmental Science Physics Social Sciences

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Geological Identification of Seismic Source at Opak Fault Based on Stratigraphic Sections of the Southern Mountains Pandita, Hita; Sukartono, Sukartono; Isjudarto, Agustinus
Forum Geografi Vol 30, No 1 (2016): July 2016
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v30i1.1508

Abstract

Earthquake is one of the unpredicted natural disasters on our earth. Despite of the absence of high-accuracy method to precisely predict the occurrence of earthquake, numerous studies have been carried out by seismologists to find it. One of the efforts to address the vulnerability of a region to earthquakes is by recognizing the type of rock as the source of the earthquake. Opak Fault is an active fault which was thought to be the source of earthquakes in Yogyakarta and adjacent areas. This study aimed to determine the seismic source types of rocks in Yogyakarta and adjacent areas. The methods were by measuring stratigraphic sections and the layer thickness in the western part of Southern Mountains. Field study was done in 6 (six) research sites. Results of stratigraphic measurement indicated the sedimentary rocks in the Southern Mountains was 3.823 km in thick, while the bedrock was more than 1.042 km in thick. Based on the result, the rock types as the seismic source were thought to originate from the continental crust rocks formed of granite and metamorphic complex.
Identification and Stratiraphic Position of Mollusk Type Locality at West Progo Stage Hita Pandita; Gendoet Hartono
Journal of Geoscience, Engineering, Environment, and Technology Vol. 4 No. 2 (2019): JGEET Vol 04 No 02 : June (2019)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (651.292 KB) | DOI: 10.25299/jgeet.2019.4.2.2682

Abstract

The location of the discovery of mollusk fossils on the island of Java is spread in various places. One location is in the Kulon Progo region known as West Progo beds. However, due to the lack of studies of mollusk fossils in the Kulon Progo region, this resulted in a lack of understanding of the location of the discovery. This study was intended to re-record the location of fossil molluscs discovery in the Kulon Progo region, with the aim of contributing to the stratigraphic arrangement in Kulon Progo. Research methods include literature studies, field investigations and laboratory analysis. The literature study includes libraries of the Dutch colonial era regarding the location of the discovery of mollusk fossils. Field studies in the form of stratigraphic measurements and sampling. Laboratory investigations include petrographic observations and identification of micro and macro fossils. The results of the investigation successfully re-identified the Kembang Sokkoh and Spolong locations which are two types of locations on the West Progo beds. Based on the lithological characteristics of the two locations included in the Jonggrangan Formation, with the Lower Miocene age based on an analysis of the fossil content of the molluscs.
GRANULOMETRIC MODELS OF ZARIA BANTAMENSIS BEDS AT BOJONG AND BAYAH AREA, IN BANTEN PROVINCE Hita Pandita
KURVATEK Vol 4 No 1 (2019): Reka Ruang
Publisher : Institut Teknologi Nasional Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33579/krvtk.v4i1.1131

Abstract

Several research on mollusk fossils have been done in Indonesia. So far research was focused in the identification of species. Although thestudy ofrelationshipsbetween mollusks fossilsand their environment is important, only a few studies have been carried out it in Indonesia. The present study is aimed to reveal the relationships of genus Zaria appearance and sedimentation mechanism and expected to provide an overview of environmental model of Zaria. The methods used are field surveys, laboratory analysis and identification of morphological character of Zaria. Field surveys were conducted in two sites of discovery of Zaria bantamensis fossil in Bayah and Bojong areas. Laboratory work composes of granulometricand statistical analysis of biometric Zaria.The results showed that Zaria bantamensis appeareancewas associated with the rocks of poor sorting characteristics, with medium to fine sand grain sizes. Based on Visher curve the sedimentation mechanism of Bojong samples was dominated by saltation and in Bayah samples was thesuspensions. The results also indicate a possible relationship between shell length and sedimentation mechanism conditions.
Evolution of T. simplex, Jenkins from the Middle Miocene to the Early Pliocene and its Chances of Becoming a Distinct Subspecies Pandita, Hita; Al Hussein Flower Risqy
Journal of Geoscience, Engineering, Environment, and Technology Vol. 9 No. 2 (2024): JGEET Vol 09 No 02 : June (2024)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2024.9.2.14331

Abstract

The presence of Turritellidae fossils in rocks is very important, because they are index fossils at the levels of mollusk biostratigraphy in Indonesia. However, its use is not yet optimal, due to one of the reasons being different names for the same specimen or conversely giving the same species name to different forms. One example is Turritella simplex. This research is intended to re-identify Turritella simplex originating from two populations that have different shapes and sizes. The goal is to find out whether the two populations are the same or different species. The method used is the analysis of the similarity of the identification parameters and the similarity test of the biometric patterns. The results showed that the two populations from Cilanang and Meningten showed similar morphological identification parameters, but differen in biometric aspects. The recommendation from this research is to divide it into two different subspecies, and can be represented at different biostratigraphic levels. Both populations show an evolutionary process in terms of biometry and morphology.
Prediksi Jarak Lemparan Flyrock pada Aktivitas Peledakan Overburden Tambang Batubara di PIT 110 IUP PT. Kemilau Rindang Abadi Rifai, Achmad; Wijaya, R. A. E.; Pandita, Hita
Jurnal Geosains dan Teknologi Vol 8, No 2 (2025)
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/jgt.8.2.2025.85-92

Abstract

Lokasi penelitian berada di Pit 110 IUP PT. Kemilau Rindang Abadi yang merupakan lokasi pertambangan batubara, dengan aktivitas peledakan sebagai metoda utama dalam memberai overburden. Namun, aktivitas peledakan berpotensi menyebabkan kerugian apabila flyrock mengenai alat atau manusia, sehingga perlu diperhitungkan prediksi lemparan flyrock. Tujuan penelitian untuk mengetahui nilai prediksi jarak lemparan flyrock, dan mengetahui korelasi parameter-parameter peledakan yang berpengaruh terhadap jarak lemparan flyrock. Metoda penelitian yang digunakan pada penelitian ini yaitu metoda kuantitatif dengan menghitung rumusan prediksi jarak lemparan flyrock yang dibandingkan dengan jarak aktual flyrock yang diukur menggunakan GPS handheld dan meteran. Berdasarkan perhitungan prediksi Richard dan Moore dihasilkan nilai deviasi yang sangat tinggi dengan hasil perhitungan metoda face burst memiliki penyimpangan sebesar 118,01 m (93%), cratering 90,60 m (69%), dan rifling 97,01 m (74%), kemudian perhitungan prediksi Ebrahim Ghasemi dengan perhitungan analisis dimensi dihasilkan nilai dengan tingkat keakuratan paling tinggi yaitu 77% dengan penyimpangan sebesar 28,7 m (23%) yang dijadikan rekomendasi perhitungan prediksi jarak flyrock. Berdasarkan hasil analisis regresi linier diketahui parameter yang dapat dikontrol dari tingkatan tertinggi hingga terendah yaitu kedalaman (R2=0,8024), burden (R2=0,7433), water content (R=0,6734), dan powder factor (R=0,6292), dan spacing (R2=0,0061).
Analisis Batugamping Sebagai Bahan Baku Semen Di Desa Gombang Kabupaten Gunung Kidul Hardiyanto, Dwi Wahyu; Pandita, Hita
Jurnal Geosains dan Teknologi Vol 8, No 2 (2025)
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/jgt.8.2.2025.124-130

Abstract

The Wonosari Formation is composed of reef limestone, which possesses excellent qualifications as raw material for cement production. However, the presence of the Gunung Sewu Geopark has limited the permissible mining areas, making it interesting to study its potential not only as cement raw material but also for other products. The quality and quantity levels of the limestone are of significant importance in both scientific and industrial contexts. The genesis of the limestone in the study area consists of muddy allochem limestone and muddy micrite. Porosity tests indicate that the limestone has a generally moderate to good porosity level, ranging from 15% to 20%, with dominant structures of vug and channel types. Chemically, it meets the standard requirements for economically viable cement raw material, with SiO₂, Al₂O₃, Fe₂O₃, MgO, and SO₃ contents below 5%, and CaO content above 50%.
Co-Authors ACHMAD RIFAI Agustinus Isjudarto Al Hussein Flower Risqy Hardiyanto, Dwi Wahyu Hill Gendoet Hartono Sukartono Sukartono Wijaya, R. A. E.