Abstract
Gravity data acquired from Cheshire basin located in the northwestern part of the United Kingdom were processed and analysed to determine the structural pattern within the entire sedimentary basin. A total of 753 gravity data were obtained from the British Geological Society and with the aid of Oasis Montaj software, maps of Bouguer anomaly, isostatic and total horizontal derivative were obtained for qualitative and quantitative interpretation in determining the fault trend and the tectonic system of the study area. The positive Bouguer anomaly region found in the northwest of the study area is associated with the high density sedimentary rocks while the negative region in the southern part corresponds to low density sediments. The regional and local isostatic maps with different cut-off wavelengths reflect changes in anomalies corresponding to different types of sedimentary rocks. The general trends of faults in the Chesire basin are shown in the total horizontal derivative map of the Bouguer gravity values. Most of the major faults found in the southern part of the study area are trending in NW-SE and NE-SW directions. The less dominant faults are found in the western and eastern parts with N-S trending faults while in the northern and southern part are trending E-W. The 2D modeling shows the estimated depth to limestone basement of about 3736 m below the sandstone and mudstone.
| Original language | English |
|---|---|
| Title of host publication | 2014 UKM FST Postgraduate Colloquium - Proceedings of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology 2014 Postgraduate Colloquium |
| Editors | Zahari Ibrahim, Haja Maideen Kader Maideen, Nazlina Ibrahim, Nurul Huda Abd Karim, Taufik Yusof, Fatimah Abdul Razak, Nurulkamal Maseran, Rozida Mohd Khalid, Noor Baa'yah Ibrahim, Hasidah Mohd. Sidek, Mohd Salmi Md Noorani, Norbert Simon |
| Publisher | American Institute of Physics Inc. |
| Pages | 644-650 |
| Number of pages | 7 |
| ISBN (Electronic) | 9780735412507 |
| DOIs | |
| Publication status | Published - 1 Jan 2014 |
| Event | 2014 Postgraduate Colloquium of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology, UKM FST 2014 - Selangor, Malaysia Duration: 9 Apr 2014 → 11 Apr 2014 |
Publication series
| Name | AIP Conference Proceedings |
|---|---|
| Volume | 1614 |
| ISSN (Print) | 0094-243X |
| ISSN (Electronic) | 1551-7616 |
Other
| Other | 2014 Postgraduate Colloquium of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology, UKM FST 2014 |
|---|---|
| Country | Malaysia |
| City | Selangor |
| Period | 9/4/14 → 11/4/14 |
Fingerprint
Keywords
- 2D modeling
- Cheshire basin
- Gravity anomaly
- Oasis montaj software
ASJC Scopus subject areas
- Physics and Astronomy(all)
Cite this
Analysis Of cheshire basin by gravity method : Some preliminary results. / Shafie, Nadiah Hanim; Hamzah, Umar; Samsudin, Abdul Rahim.
2014 UKM FST Postgraduate Colloquium - Proceedings of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology 2014 Postgraduate Colloquium. ed. / Zahari Ibrahim; Haja Maideen Kader Maideen; Nazlina Ibrahim; Nurul Huda Abd Karim; Taufik Yusof; Fatimah Abdul Razak; Nurulkamal Maseran; Rozida Mohd Khalid; Noor Baa'yah Ibrahim; Hasidah Mohd. Sidek; Mohd Salmi Md Noorani; Norbert Simon. American Institute of Physics Inc., 2014. p. 644-650 (AIP Conference Proceedings; Vol. 1614).Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Analysis Of cheshire basin by gravity method
T2 - Some preliminary results
AU - Shafie, Nadiah Hanim
AU - Hamzah, Umar
AU - Samsudin, Abdul Rahim
PY - 2014/1/1
Y1 - 2014/1/1
N2 - Gravity data acquired from Cheshire basin located in the northwestern part of the United Kingdom were processed and analysed to determine the structural pattern within the entire sedimentary basin. A total of 753 gravity data were obtained from the British Geological Society and with the aid of Oasis Montaj software, maps of Bouguer anomaly, isostatic and total horizontal derivative were obtained for qualitative and quantitative interpretation in determining the fault trend and the tectonic system of the study area. The positive Bouguer anomaly region found in the northwest of the study area is associated with the high density sedimentary rocks while the negative region in the southern part corresponds to low density sediments. The regional and local isostatic maps with different cut-off wavelengths reflect changes in anomalies corresponding to different types of sedimentary rocks. The general trends of faults in the Chesire basin are shown in the total horizontal derivative map of the Bouguer gravity values. Most of the major faults found in the southern part of the study area are trending in NW-SE and NE-SW directions. The less dominant faults are found in the western and eastern parts with N-S trending faults while in the northern and southern part are trending E-W. The 2D modeling shows the estimated depth to limestone basement of about 3736 m below the sandstone and mudstone.
AB - Gravity data acquired from Cheshire basin located in the northwestern part of the United Kingdom were processed and analysed to determine the structural pattern within the entire sedimentary basin. A total of 753 gravity data were obtained from the British Geological Society and with the aid of Oasis Montaj software, maps of Bouguer anomaly, isostatic and total horizontal derivative were obtained for qualitative and quantitative interpretation in determining the fault trend and the tectonic system of the study area. The positive Bouguer anomaly region found in the northwest of the study area is associated with the high density sedimentary rocks while the negative region in the southern part corresponds to low density sediments. The regional and local isostatic maps with different cut-off wavelengths reflect changes in anomalies corresponding to different types of sedimentary rocks. The general trends of faults in the Chesire basin are shown in the total horizontal derivative map of the Bouguer gravity values. Most of the major faults found in the southern part of the study area are trending in NW-SE and NE-SW directions. The less dominant faults are found in the western and eastern parts with N-S trending faults while in the northern and southern part are trending E-W. The 2D modeling shows the estimated depth to limestone basement of about 3736 m below the sandstone and mudstone.
KW - 2D modeling
KW - Cheshire basin
KW - Gravity anomaly
KW - Oasis montaj software
UR - http://www.scopus.com/inward/record.url?scp=85063857841&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85063857841&partnerID=8YFLogxK
U2 - 10.1063/1.4895278
DO - 10.1063/1.4895278
M3 - Conference contribution
AN - SCOPUS:85063857841
T3 - AIP Conference Proceedings
SP - 644
EP - 650
BT - 2014 UKM FST Postgraduate Colloquium - Proceedings of the Universiti Kebangsaan Malaysia, Faculty of Science and Technology 2014 Postgraduate Colloquium
A2 - Ibrahim, Zahari
A2 - Maideen, Haja Maideen Kader
A2 - Ibrahim, Nazlina
A2 - Karim, Nurul Huda Abd
A2 - Yusof, Taufik
A2 - Razak, Fatimah Abdul
A2 - Maseran, Nurulkamal
A2 - Khalid, Rozida Mohd
A2 - Ibrahim, Noor Baa'yah
A2 - Sidek, Hasidah Mohd.
A2 - Noorani, Mohd Salmi Md
A2 - Simon, Norbert
PB - American Institute of Physics Inc.
ER -