Seismic Sequence Stratigraphic Sub-Division Using Well Logs and Seismic Data of Taranaki Basin, New Zealand
العنوان: | Seismic Sequence Stratigraphic Sub-Division Using Well Logs and Seismic Data of Taranaki Basin, New Zealand |
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المؤلفون: | Mohamed Elsaadany, Ismailalwali A. M. Babikir, Teslim Adeleke, Mohammed Ali Mohammed Al-Bared, Umar Hamzah, Abd Al-Salam Al-Masgari, Abdul Halim Abdul Latiff, Qazi Sohail Imran, Maman Hermana |
المصدر: | Applied Sciences Volume 11 Issue 3 Applied Sciences, Vol 11, Iss 1226, p 1226 (2021) |
بيانات النشر: | Multidisciplinary Digital Publishing Institute, 2021. |
سنة النشر: | 2021 |
مصطلحات موضوعية: | 010504 meteorology & atmospheric sciences, Well logging, 010502 geochemistry & geophysics, lcsh:Technology, 01 natural sciences, lcsh:Chemistry, Sedimentary depositional environment, Paleontology, Sequence (geology), General Materials Science, Sequence stratigraphy, lcsh:QH301-705.5, Instrumentation, 0105 earth and related environmental sciences, Fluid Flow and Transfer Processes, Feature (archaeology), seismic facies classification, lcsh:T, Process Chemistry and Technology, seismic sequence stratigraphy, General Engineering, Taranaki Basin, and isochron maps, lcsh:QC1-999, Computer Science Applications, lcsh:Biology (General), lcsh:QD1-999, lcsh:TA1-2040, Section (archaeology), Period (geology), lcsh:Engineering (General). Civil engineering (General), lcsh:Physics, Geology, taranaki basin |
الوصف: | This study focuses on the sequence stratigraphy and the dominated seismic facies in the Central Taranaki basin. Four regional seismic sequences namely SEQ4 to SEQ1 from bottom to top and four boundaries representing unconformities namely H4 to H1 from bottom to top have been traced based on the reflection terminations. This was validated using well logs information. An onlapping feature on the seismic section indicates a new perspective surface separated between the upper and lower Giant formation, which indicates a period of seawater encroachment. This study focused extensively on deposition units from SEQ4 to SEQ1. The seismic facies, isochron map, and depositional environment were determined, and the system tract was established. This study was also able to propose a new perspective sequence stratigraphy framework of the basin and probable hydrocarbon accumulations and from the general geological aspect, SA-Middle Giant Formation (SEQ3) could act as potential traps. |
وصف الملف: | application/pdf |
اللغة: | English |
تدمد: | 2076-3417 |
DOI: | 10.3390/app11031226 |
الوصول الحر: | https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2334ae52660ea0713593d4cab85dca93Test |
حقوق: | OPEN |
رقم الانضمام: | edsair.doi.dedup.....2334ae52660ea0713593d4cab85dca93 |
قاعدة البيانات: | OpenAIRE |
تدمد: | 20763417 |
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DOI: | 10.3390/app11031226 |