scholarly journals GEOSPATIAL APPROACH FOR GEOLOGICAL INVESTIGATION AT DISTRICT OF MERSING

2021 ◽  
Vol 6 (24) ◽  
pp. 174-185
Author(s):  
Muhamad Asyraf Zamari ◽  
Tajul Ariffin Musa ◽  
Edy Tonnizam Mohamad ◽  
Ivin Amri Musliman ◽  
Wan Anom Wan Aris
Keyword(s):  
Control Point ◽  
Geological Structure ◽  
Geological Mapping ◽  
Structure Mapping ◽  
Geospatial Information ◽  
Geological Investigation ◽  
Precision Control ◽  
Gps Positioning ◽  
Gps Measurement ◽  
Geological Information

Effective geological information evaluation is essential for accurate site characterization. A major concern in geological mapping is to locate the accurate location of the geological information. The geoinformation approach such as precise GPS surveying and UAV mapping could be integrated with other geospatial information to augment the geological information. This research aims to integrate the geoinformation approach into geological structure mapping. To achieve the overall purpose of the study, the objective identified was the establishment of a high-precision control point by using Precise GPS measurement in the study area. Therefore, the establishment of GPS data observations involves the establishment of primary networks and several GPS controls points within the study area. Subsequently, the GPS positioning has been processed to produce a topographic information map and to support the collection of geological data in the study area. It is hoped that the integration of the geoinformation approach has been provided a significant increase in geological information at the district of Mersing.

scholarly journals KAJIAN GEOLOGI TERHADAP SITUS-SITUS DI PEKALONGAN, PROVINSI JAWA TENGAH (Geological Study On Sites In Pekalongan, Central Java Province)

2019 ◽  
Vol 11 (1) ◽  
pp. 1-18
Author(s):  
Muh. Fadhlan Syuaib Intan
Keyword(s):  
Research Area ◽  
Geological Structure ◽  
Geological Mapping ◽  
Archaeological Sites ◽  
Geological Structures ◽  
Main Research ◽  
Central Java ◽  
Intermittent Rivers ◽  
Geological Information ◽  
Research Problems

Pekalongan the study location, present many cultural remains, one of which is from the Hindu-Buddhist period, which has not gotten any attention of environmental researchers yet. This becomes the basis of the main research problems that cover geology in general. Therefore, the purpose of this research is to carry out surface geological mapping in general as one of the efforts to present geological information, while the aim is to find out the geomorphological aspects, stratigraphy, geological structures that are associated with the existence in archaeological sites of the research area. The research method begins with literature review, surveys, analysis, and interpretation of field data. Environmental observation provides information about the landscape consisting of terrestrial morphology units, weak corrugated morphological units, and strong corrugated morphological units. The river is dendritic, radial and rectangular patterned, with the old-mature river and the old river, periodic/permanent rivers, and episodic/intermittent rivers. The rock Compositions are alluvial, andesite, basalt, volcanic breccias, and sandstones. The geological structure is in the form of faults, and is joint. The exploration in Pekalongan has found six Hindu-Buddhist sites. ABSTRAKPekalongan, yang menjadi lokasi penelitian, menyimpan banyak tinggalan budaya, salah satunya dari masa Hindu-Budha, yang belum mendapat perhatian dari para peneliti lingkungan. Hal inilah yang dijadikan dasar permasalahan utama penelitian yang mencakup geologi secara umum. Oleh sebab itu, maksud penelitian ini adalah untuk melakukan pemetaan geologi permukaan secara umum sebagai salah satu upaya untuk menyajikan informasi geologi, sedangkan tujuannya adalah untuk mengetahui aspek-aspek geomorfologi, stratigrafi, struktur geologi yang dikaitkan dengan keberadaan di situs-situs arkeologi wilayah penelitian. Metode penelitian diawali dengan kajian pustaka, survei, dan dilanjutkan dengan analisis, dan interpretasi data lapangan. Pengamatan lingkungan memberikan informasi tentang bentang alamnya terdiri yang dari satuan morfologi dataran, satuan morfologi bergelombang lemah, dan satuan morfologi bergelombang kuat. Sungainya berpola dendritik, radial, dan rektangular, berstadia sungai dewasa-tua dan sungai tua, sungai periodik/ permanen, dan sungai episodik/intermittent. Batuan penyusun adalah aluvial, andesit, basal, breksi vulkanik, dan batupasir. Struktur geologi berupa sesar, dan kekar. Eksplorasi di Kabupaten Pekalongan telah menemukan enam situs Hindu-Budha.

FEATURES OF GEOLOGICAL STRUCTURE AND PETROLEUM OIL POTENTIAL OF VICHULOVSKAYA FORMATION WITHIN VOSTOCHNO-KAMENNYI DEPOSIT (WESTERN SIBERIA)

2018 ◽  
pp. 33-39
Author(s):  
R. R. Gabdullin ◽  
O. N. Biryukova ◽  
R. A. Akhmedov
Keyword(s):  
Western Siberia ◽  
Geological Structure ◽  
Test Results ◽  
Geological Information ◽  
Petroleum Oil

The analysis of geological and geophysical materials in order to study the peculiarities of the geological structure of the Vikulov Formation within the Vodorazdel license area was carried out. The presented factual material makes it possible to characterize the geological structure of the investigated area more informatively and for interpreting of seismic materials. The analysis of geological information (GIS and test results) confirms the approved water–oil contact (WOC) level in the investigated section of the deposit, which makes it possible to recalculate its reserves.

Walcot Gibson 1864-1941

1943 ◽  
Vol 4 (12) ◽  
pp. 271-275
Keyword(s):  
East Africa ◽  
Geological Structure ◽  
Geological Mapping ◽  
Geological Survey ◽  
Intimate Contact ◽  
The North ◽  
South Wales ◽  
New Information ◽  
Original Survey ◽  
The One

Walcot Gibson was born at Bromsgrove, Worcestershire, on 24 August 1864. His father was a bank manager from the north country and his mother was Cornish, and they had three sons and one daughter. Gibson was educated at the Bromsgrove School and about 1882 went to Mason College, Birmingham, now the University of Birmingham. Charles Lapworth who had distinguished himself by his great researches in the south of Scotland had just been appointed to the chair of Geology at Mason College and thirty-one years later (1913) he records that Gibson was his first geological pupil. His interest in geology and geological mapping was developed by intimate contact with Lapworth and was sustained by a coterie of ardent amateur geologists, among them Joseph Landon, Fred Cullis and C. J. Gilbert. This period clearly determined Gibson’s choice of a career. After a course at the Royal College of Science he set out in 1889 on Lapworth’s advice for South Africa where he was engaged for two years on mineral surveys in the Rand goldfields and elsewhere. From there he moved to East Africa where he was engaged for another two years on mineral surveys for the East Africa Company. He returned to this country an experienced geologist and surveyor and in 1893 he joined H.M. Geological Survey in which service he remained for thirty-two years until his retirement in 1925. This was an important period in the history of the Geological Survey for owing to strong representations that the old Survey had become obsolete both in topography and geology, the House of Commons in 1891 sanctioned a resurvey of the great South Wales Coalfield on the scale of six inches to the mile. The first mapping of that field initiated by Logan and de la Beche was on the one-inch scale and was completed about 1845, the year in which the Geological Survey was transferred from the Board of Ordnance. The enormous developments which had taken place since the original survey had far outstripped the knowledge of the geological structure of the field and new information had become urgently necessary.

scholarly journals New insights into the geological structure of the Netherlands; results of a detailed mapping project

2012 ◽  
Vol 91 (4) ◽  
pp. 419-446 ◽  
Author(s):  
H. Kombrink ◽  
J.C. Doornenbal ◽  
E.J.T. Duin ◽  
M. den Dulk ◽  
J.H. ten Veen ◽  
...  
Keyword(s):  
Standard Deviation ◽  
The Netherlands ◽  
Seismic Data ◽  
Geological Structure ◽  
Geological Mapping ◽  
3D Seismic ◽  
Structural Element ◽  
Potential Reservoir ◽  
3D Seismic Data ◽  
New Reservoir

AbstractA five years geological mapping project, in which the Netherlands Continental Shelf has been re-examined using all publicly available data, resulted in an important update of the existing dataset. The stratigraphy of over 400 wells has been re-interpreted. New depth and thickness grids, based mainly on the interpretation of 3D seismic data have been produced for the most important stratigraphic intervals from Permian Upper Rotliegend to Neogene. New reservoir grids describe the top, base and thickness of 30 (potential) reservoir units in the area. In addition, the uncertainty related to interpretation and further processing of the data has been assessed. This resulted in maps displaying the standard deviation for the depth of the main stratigraphic intervals. Based on these results and the data already available for the onshore area, an updated structural element map was made for the Netherlands.

Use of geological mapping tools to improve the hydraulic performance of SuDS

2015 ◽  
Vol 71 (10) ◽  
pp. 1492-1499 ◽  
Author(s):  
Britta Bockhorn ◽  
Knud Erik Strøyberg Klint ◽  
Marina Bergen Jensen ◽  
Ingelise Møller
Keyword(s):  
Hydraulic Performance ◽  
Electrode System ◽  
Geological Mapping ◽  
Geological Heterogeneity ◽  
Shallow Subsurface ◽  
Glacial Origin ◽  
Infiltration Rates ◽  
Geological Information ◽  
Infiltration Tests ◽  
Subsurface Resistivity

Most cities in Denmark are situated on low permeable clay rich deposits. These sediments are of glacial origin and range among the most heterogeneous, with hydraulic conductivities spanning several orders of magnitude. This heterogeneity has obvious consequences for the sizing of sustainable urban drainage systems (SuDS). We have tested methods to reveal geological heterogeneity at field scale to identify the most suitable sites for the placement of infiltration elements and to minimize their required size. We assessed the geological heterogeneity of a clay till plain in Eastern Jutland, Denmark measuring the shallow subsurface resistivity with a geoelectrical multi-electrode system. To confirm the resistivity data we conducted a spear auger mapping. The exposed sediments ranged from clay tills over sandy clay tills to sandy tills and correspond well to the geoelectrical data. To verify the value of geological information for placement of infiltration elements we carried out a number of infiltration tests on geologically different areas across the field, and we observed infiltration rates two times higher in the sandy till area than in the clay till area, thus demonstrating that the hydraulic performance of SuDS can be increased considerably and oversizing avoided if field geological heterogeneity is revealed before placing SuDS.

scholarly journals Account of the Progress of the Geological Survey in Scotland, illustrated by Maps and Sections

1866 ◽  
Vol 5 ◽  
pp. 355-364
Author(s):  
Archibald Geikie
Keyword(s):  
United Kingdom ◽  
Geological Structure ◽  
Small Degree ◽  
Geological Mapping ◽  
Geological Survey ◽  
The United Kingdom

The object of the Geological Survey is to ascertain in detail the geological structure of the United Kingdom, and to publish the results in maps, sections, and descriptive memoirs. The Ordnance maps form the groundwork on which these geological investigations proceed; and as no district is examined until these maps are ready, the progress of the Geological Survey is guided in no small degree by that of the Ordnance engineers. In Scotland, the geological mapping has hitherto been conducted wholly upon the county maps on the scale of six inches to a mile, and the advantages of so large a scale are such, that although the work is finally reduced and published on the scale of one inch to a mile, no county is surveyed until its six-inch maps are ready for use.

scholarly journals Evaluasi Kondisi Geologi Teknik dalam Pembangunan Embung

2019 ◽  
Vol 5 (1) ◽  
pp. 121
Author(s):  
I Gde Budi Indrawan ◽  
Shinta Dwi Novianti ◽  
Heru Hendrayana ◽  
Doni Prakasa Eka Putra ◽  
Wahyu Wilopo
Keyword(s):  
Water Source ◽  
Geological Structure ◽  
Source Location ◽  
Geological Mapping ◽  
Engineering Geological Mapping ◽  
Merapi Volcano ◽  
Geomorphic Process ◽  
Geological Conditions ◽  
Detention Pond ◽  
Impermeable Layer

Pucang Village was consisted of eruption materials of Merapi Volcano. The relatively high coefficient of permeability of the materials consisting this area caused rainwater to directly infiltrate into the ground. Evaluation of engineering geological conditions was conducted for construction of a detention pond in this area, which had limited water supply for daily activities. The evaluation was conducted on results of a 1:10.000 scale of engineering geological mapping and analyses of 1:10.000 scale of geological disaster maps produced by previous researchers. The engineering geological mapping involved mapping of morphological condition and active geomorphic process, lithological condition, existence of geological structure, and water source location. The evaluation results showed that the proposed location met the land suitability criteria for detention pond construction based on the morphological condition and active geomorphic process, existence of geological structure, and water source location, but did not meet those based on the lithological and vulnerability to Merapi Volcano eruption disaster. Construction of impermeable layer to prevent water seepage into the ground and periodic removal of sediment in the base of the detention pond were suggested to be carried out to keep the detention pond functioning properly.

scholarly journals GEOARKEOLOGI CEKUNGAN SOA, FLORES, NUSA TENGGARA TIMUR

Siddhayatra ◽  
2019 ◽  
Vol 23 (1) ◽  
pp. 31
Author(s):  
Fadhlan Syuaib Intan
Keyword(s):  
Normal Fault ◽  
Geological Structure ◽  
Raw Material ◽  
Alluvial Deposits ◽  
Fault Type ◽  
Geological Conditions ◽  
Geological Information ◽  
Surrounding Areas ◽  
Field Data Analysis ◽  
Surface Geology

Cekungan Soa yang termasuk wilayah Kabupaten Ngada dan Kabupaten Nagekeo terletak di Pulau Flores, banyak menyimpan tinggalan budaya yang antara lain berasal dari masa Paleolitik, yang selama ini belum terlalu diperhatikan oleh peneliti lingkungan, khususnya geoarkeologi. Hal inilah yang menjadi pokok permasalahan yang mencakup kondisi geologi secara umum. Adapun maksud penelitian ini adalah melakukan pemetaan geologi permukaan secara umum sebagai salah satu upaya menyajikan informasi geologi terkait dengan situs arkeologi. Tujuannya adalah untuk mengetahui aspek-aspek geomorfologi, stratigrafi di situs-situs arkeologi. Metode penelitian dilakukan melalui kajian pustaka, survei, analisis data lapangan dan interpretasi. Pengamatan lingkungan memberikan informasi tentang bentang alam daerah penelitian yang terdiri dari satuan morfologi dataran, dan satuan morfologi bergelombang lemah. Sungainya berpola aliran centripetal, berstadia Sungai Dewasa-Tua, sungai tua, Sungai Periodik/Permanen, dan Sungai Episodik/Intermittent. Batuan penyusun adalah breksi vulkanik, tufa, konglomerat, dan endapan aluvial. Struktur geologi berupa patahan dari jenis patahan normal. Eksplorasi di Cekungan Soa telah mendata 12 situs paleolitik. Dari klasifikasi petrologi, alat-alat litik terbuat dari batuan jasper, chert, andesit, dan basal. Batuan sebagai bahan baku alat litik, banyak ditemukan di Cekungan Soa dan sekitarnya, baik dalam bentuk singkapan maupun boulder. Kata kunci: geologi, plistosen, paleolitik, situs terbuka, bahan alat litikSoa Basin, which belongs to Ngada Regency and Nagekeo Regency, is located on Flores Island, with many cultural stays, among others, from the Paleolithic period, which has not been too concerned by environmental researchers, especially geoarkeology. This is the issue that covers general geological conditions. The purpose of this research is to mapping the surface geology in general as an effort to present geological information related to archeological site. The aim is to know the geomorphological, stratigraphic aspects of the archaeological sites. The research method is done through literature review, survey, field data analysis and interpretation. Environmental observations provide information on the landscape of the study area consisting of terrestrial morphology units, and weak wavy morphology units. The river is centripetal flow pattern, with the old river, mature-old river, periodic/permanent river, and episodik /intermittent river. Constituent rocks are volcanic breccias, tuffs, conglomerates, and alluvial deposits. The geological structure is a fracture of the normal fault type. Exploration in the Soa Basin has listed 12 paleolithic sites. From the classification of petrology, litik tools made of jasper, chert, andesite, and basalt rocks. Rock as a raw material litik, found in Soa Basin and surrounding areas, both in the form of outcrops and boulder. Keywords: geology, pleistocene, paleolithic, open site, lithic tools materials

scholarly journals GEOLOGY AND PETROGRAPHY OF THE VEDEL ISLANDS (WILHELM ARCHIPELAGO, WEST ANTARCTICA)

2020 ◽  
pp. 18-27
Author(s):  
O. Mytrokhyn ◽  
V. Bakhmuto
Keyword(s):  
Large Scale ◽  
Deep Level ◽  
Geological Structure ◽  
Geological Mapping ◽  
Small Island ◽  
West Antarctica ◽  
Mode Of Occurrence ◽  
Plutonic Rocks ◽  
The Antarctic ◽  
Tectonic Exhumation

The Vedel Islands are a small island group that is part of the Wilhelm archipelago in the West Antarctica. They are located near the Graham Coast of the Antarctic Peninsula at a distance of 12 km from Akademik Vernadsky Ukrainian Antarctic Station. Until recently, the Vedel Islands were a "white spot" on all existing geological maps. In 2019, during the seasonal work of the 24th Ukrainian Antarctic expedition, the authors first carried out field geological researches on the Vedel Islands. The main goal of the geological survey was reconnaissance and large-scale geological mapping. The general ideas about the geological structure of the study area were developed by further processing of the collected materials. The preliminary data about the mode of occurrence, the geological ages, the petrographic peculiarities and the ore potential of the local rocks were also obtained. It was first established that multiple-aged intrusive-magmatic formations take part in the geological structure of the Vedel Islands. The intermediate compositions of the plutonic rocks namely the diorites and quartz diorites are the most common among them. The gabbroids and the tonalites are less common. The least common ones are hypabyssal and subvolcanic dike rocks namely microdiorites and diabases. The plutonic rocks were formed in at least three intrusive phases with a homodromous order of their intrusions. The most ancient among them are gabbroids. The Early Cretaceous age for their formation is assumed by analogy with the petrographically similar rocks of the Tuxen-Rasmussen layered gabbroid intrusion (TRGI). The tonilites are the youngest plutonic rocks on the Vedel Islands. It is assumed that their formation at a deep level took place in the Late Cretaceous, although their tectonic exhumation and the final erosion outcropping occurred in the Paleogene and ended in the Neogene. In the process of the exhumation, the plutonic rocks were intruded by hypabyssal dikes of microdiorites. The youngest subvolcanic diabase dykes intruded the tonalites supposedly after their complete erosion outcropping i. e. in Neogene or even Quaternary. Like TRGI and other layered gabbroid intrusions of the Wilhelm archipelago, the Vedel island gabbroids contain iron-titanium oxide-ore and copper-silicate mineralization, which requires further study. The additional researches are also needed to clarify the age, origin, petrography and mineralogy of the numerous veins of aplite-pegmatoid granite which intrude gabbroids and diorites on the Vedel Islands.

Sign in / Sign up

Export Citation Format

Share Document