Seismic study of the mud diapir structures in the Okinawa Trough
In the Okinawa Trough, a number of mud diapirs were observed by the seismic datasets from several different cruises. In this paper, based on the seismic profiles, we separated three different types of mud diapirs according to their configuration. All the mud diapirs are associated with free gas or g...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Xing, Junhui [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Rechteinformationen: |
Nutzungsrecht: Copyright © 2016 John Wiley & Sons, Ltd. |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Geological journal - Chichester : Wiley, 1964, 51(2016), S1, Seite 203-208 |
|---|---|
| Übergeordnetes Werk: |
volume:51 ; year:2016 ; number:S1 ; pages:203-208 |
| Links: |
|---|
| DOI / URN: |
10.1002/gj.2824 |
|---|
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| 520 | |a In the Okinawa Trough, a number of mud diapirs were observed by the seismic datasets from several different cruises. In this paper, based on the seismic profiles, we separated three different types of mud diapirs according to their configuration. All the mud diapirs are associated with free gas or gas hydrates, indicating that the mud diapirs could sever good migration pathways for free gas migrating upwards. Mud diapirs are distributed in the middle and south of the Okinawa Trough. Most of them are located to the south of the Miyako Fault zone. The triggering mechanisms were discussed in a large scale, which suggests the mud diapirs might be triggered by the collision between the Eurasian Plate and the northward subducting Philippine Luzon arc. The distribution of mud diapirs was mainly controlled by the compression during the Late Miocene and the Miyako Fault zone. Copyright © 2016 John Wiley & Sons, Ltd. | ||
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10.1002/gj.2824 doi PQ20161012 (DE-627)OLC1981633707 (DE-599)GBVOLC1981633707 (PRQ)p1174-b4f06961ec216db8694c15e4267324117d4ffc47422dc95e91601f0f1a8dabef3 (KEY)0040727520160000051000000203seismicstudyofthemuddiapirstructuresintheokinawatr DE-627 ger DE-627 rakwb eng 550 ZDB 38.10 bkl Xing, Junhui verfasserin aut Seismic study of the mud diapir structures in the Okinawa Trough 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier In the Okinawa Trough, a number of mud diapirs were observed by the seismic datasets from several different cruises. In this paper, based on the seismic profiles, we separated three different types of mud diapirs according to their configuration. All the mud diapirs are associated with free gas or gas hydrates, indicating that the mud diapirs could sever good migration pathways for free gas migrating upwards. Mud diapirs are distributed in the middle and south of the Okinawa Trough. Most of them are located to the south of the Miyako Fault zone. The triggering mechanisms were discussed in a large scale, which suggests the mud diapirs might be triggered by the collision between the Eurasian Plate and the northward subducting Philippine Luzon arc. The distribution of mud diapirs was mainly controlled by the compression during the Late Miocene and the Miyako Fault zone. Copyright © 2016 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2016 John Wiley & Sons, Ltd. Okinawa Trough mud diapir seismic Jiang, Xiaodian oth Li, Deyong oth Enthalten in Geological journal Chichester : Wiley, 1964 51(2016), S1, Seite 203-208 (DE-627)129358908 (DE-600)160486-7 (DE-576)014731223 0072-1050 nnns volume:51 year:2016 number:S1 pages:203-208 http://dx.doi.org/10.1002/gj.2824 Volltext http://onlinelibrary.wiley.com/doi/10.1002/gj.2824/abstract http://search.proquest.com/docview/1813955056 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_65 GBV_ILN_2173 38.10 AVZ AR 51 2016 S1 203-208 |
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10.1002/gj.2824 |
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| title_sort |
seismic study of the mud diapir structures in the okinawa trough |
| title_auth |
Seismic study of the mud diapir structures in the Okinawa Trough |
| abstract |
In the Okinawa Trough, a number of mud diapirs were observed by the seismic datasets from several different cruises. In this paper, based on the seismic profiles, we separated three different types of mud diapirs according to their configuration. All the mud diapirs are associated with free gas or gas hydrates, indicating that the mud diapirs could sever good migration pathways for free gas migrating upwards. Mud diapirs are distributed in the middle and south of the Okinawa Trough. Most of them are located to the south of the Miyako Fault zone. The triggering mechanisms were discussed in a large scale, which suggests the mud diapirs might be triggered by the collision between the Eurasian Plate and the northward subducting Philippine Luzon arc. The distribution of mud diapirs was mainly controlled by the compression during the Late Miocene and the Miyako Fault zone. Copyright © 2016 John Wiley & Sons, Ltd. |
| abstractGer |
In the Okinawa Trough, a number of mud diapirs were observed by the seismic datasets from several different cruises. In this paper, based on the seismic profiles, we separated three different types of mud diapirs according to their configuration. All the mud diapirs are associated with free gas or gas hydrates, indicating that the mud diapirs could sever good migration pathways for free gas migrating upwards. Mud diapirs are distributed in the middle and south of the Okinawa Trough. Most of them are located to the south of the Miyako Fault zone. The triggering mechanisms were discussed in a large scale, which suggests the mud diapirs might be triggered by the collision between the Eurasian Plate and the northward subducting Philippine Luzon arc. The distribution of mud diapirs was mainly controlled by the compression during the Late Miocene and the Miyako Fault zone. Copyright © 2016 John Wiley & Sons, Ltd. |
| abstract_unstemmed |
In the Okinawa Trough, a number of mud diapirs were observed by the seismic datasets from several different cruises. In this paper, based on the seismic profiles, we separated three different types of mud diapirs according to their configuration. All the mud diapirs are associated with free gas or gas hydrates, indicating that the mud diapirs could sever good migration pathways for free gas migrating upwards. Mud diapirs are distributed in the middle and south of the Okinawa Trough. Most of them are located to the south of the Miyako Fault zone. The triggering mechanisms were discussed in a large scale, which suggests the mud diapirs might be triggered by the collision between the Eurasian Plate and the northward subducting Philippine Luzon arc. The distribution of mud diapirs was mainly controlled by the compression during the Late Miocene and the Miyako Fault zone. Copyright © 2016 John Wiley & Sons, Ltd. |
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| title_short |
Seismic study of the mud diapir structures in the Okinawa Trough |
| url |
http://dx.doi.org/10.1002/gj.2824 http://onlinelibrary.wiley.com/doi/10.1002/gj.2824/abstract http://search.proquest.com/docview/1813955056 |
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| author2 |
Jiang, Xiaodian Li, Deyong |
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Jiang, Xiaodian Li, Deyong |
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| up_date |
2024-07-03T14:06:30.064Z |
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