Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Itoyuki Nishioka"'
Publikováno v:
SPE Production & Operations. 32:500-516
Summary The first offshore methane-hydrate production test was conducted in the Eastern Nankai Trough area of Japan in 2013, subjecting a gas-hydrates reservoir to large drawdowns by reducing bottomhole pressure (BHP) for in-situ dissociation of gas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43be94f66a3fce1babcbdce72fc861e5
https://doi.org/10.2118/182230-pa
https://doi.org/10.2118/182230-pa
Publikováno v:
All Days.
The first offshore methane hydrate production test was conducted in the Eastern Nankai Trough area of Japan in 2013 subjecting gas hydrates reservoir to large drawdowns by reducing bottomhole pressure (BHP) for in-situ dissociation of gas hydrates. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74ac0089c05775eea3c91eded52c6fa0
https://doi.org/10.2118/182230-ms
https://doi.org/10.2118/182230-ms
Publikováno v:
Earth, Planets and Space. 59:e45-e48
Changes in the anisotropy of the low-field magnetic susceptibility (AMS) of basaltic andesite were induced by decaying stress waves and subsequently quantified. An initial shock pressure of 5 GPa was generated in a block of the target rock through im
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::749d1555044a91b81ed3e5f0f5c6e079
https://doi.org/10.1186/bf03352060
https://doi.org/10.1186/bf03352060
Publikováno v:
Polar geoscience. 18:15-25
Anisotropy of magnetic susceptibility (AMS) in deformed rocks in the Riiser-Larsen Main Shear Zone (RLMSZ) was analyzed in order to demonstrate the changes in rock magnetic properties due to deformation. Sixty-nine samples were collected at six sites
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::50d252c2ba61011c75a73811920fa9e0
http://id.nii.ac.jp/1291/00003146/
http://id.nii.ac.jp/1291/00003146/
Autor:
Itoyuki, NISHIOKA
Magnetic anomaly data provide valuable information on size and morphology of buried impact craters. An understanding of how stress waves change mag-netic properties of rock is critical for correct interpretation of magnetic data. Although previous st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::6eeee10f925a5ed611490f86de748a02
http://id.nii.ac.jp/1013/00000834/
http://id.nii.ac.jp/1013/00000834/
