ƒvƒƒOƒ‰ƒ€iŒû“ª”•\j |
”•\ŽžŠÔ |
u‰‰”Ô† |
ƒVƒ‡[ƒgƒ^ƒCƒgƒ‹ |
’˜ŽÒ |
—\eW–{•¶ |
13:10-13:25 |
A004-01 |
‚©‚®‚â“‹ÚMAP-PACE-ESA‚É‚æ‚é‚ŽžŠÔE‚‹óŠÔ•ª‰ð”\‚Å‚ÌŒŽŽ¥‹CˆÙíƒ}ƒbƒv |
ŽR–{ ’‰‹P
Ö“¡ ‹`•¶
ó‘º ˜aŽj
‚Ù‚© |
•\Ž¦ |
13:25-13:40 |
A004-02 |
’n‹…Ž¥ê‚̬ˆö-“àŠjˆ³“d‘̉¼à- |
‘ì ‹g‘¥
|
•\Ž¦ |
13:40-13:55 |
A004-03 |
Numerical dynamo model in a sphere: implications for an early dynamo action |
‚‹´ ‘¾
|
•\Ž¦ |
13:55-14:10 |
A004-04 |
’nŽ¥‹C‘SŽ¥—ÍiˆÙíj‚Ì•¨—“I‰ðÍ‚ÌŒÀŠE |
ˆÉ¨è CO
¼”ö ~
|
•\Ž¦ |
14:10-14:25 |
A004-05 |
Matuyama-Brunhes magnetic polarity transition features from Sangiran, central Java |
•º“ª K
㓈 —DŽq
¼‰Y GŽ¡
‚Ù‚© |
•\Ž¦ |
14:25-14:40 |
A004-06 |
ƒ}ƒcƒ„ƒ}]ƒuƒŠƒ…ƒ“ƒk’nŽ¥‹C‹t“]ƒgƒ‰ƒ“ƒWƒVƒ‡ƒ“‚É‚¨‚¯‚銦—≻ƒCƒxƒ“ƒg |
–kê ˆçŽq
•º“ª K
‰Á“¡ –ÎO
‚Ù‚© |
•\Ž¦ |
14:40-14:55 |
A004-07 |
ƒ^ƒqƒ`“‡‰ÎŽRŠâ‚É‚æ‚éƒuƒ‹ƒ“|¼ŽR’nŽ¥‹C‹t“]‚É‚¨‚¯‚éŒÃ’nŽ¥‹C‹“x•Ï“®‚Ì•œŒ³ |
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¬“c Œ[–M
Î’Ë Ž¡
‚Ù‚© |
•\Ž¦ |
14:55-15:10 |
A004-08 |
‘åã˜p 1700m ƒRƒA‚É‚æ‚é Gauss-Matuyama ‹«ŠE‘OŒã‚Ì’nŽ¥‹C•Ï“®•œŒ³ |
ŽO“‡ –«–¾
•º“ª K
¼‰º ‚Ü‚èŽq
‚Ù‚© |
•\Ž¦ |
15:20-15:35 |
A004-09 |
ƒ^ƒC“ì•”‚É‚¨‚¯‚éŒÃ’nŽ¥‹CŠw“IŒ¤‹† |
ŽR‰º “O
‰³“¡ —mˆê˜Y
˜a“c õ—²
‚Ù‚© |
•\Ž¦ |
15:35-15:50 |
A004-10 |
Tectonic deformation of the Indochina Peninsula recorded in the Mesozoic paleomagnetic results |
‰³“¡ —mˆê˜Y
|
•\Ž¦ |
15:50-16:05 |
A004-11 |
ŒF–쉫IODP Expedition 315‚ÅŒ@킳‚ꂽƒRƒA‚̌ÒnŽ¥‹CEŠâÎŽ¥‹C‹L˜^ |
‹à¼ •q–ç
Pares Josep
IODP‘æ315ŽŸqŠCæ‘DŒ¤‹†ŽÒˆê“¯ áÁ»‰pŽ÷
|
•\Ž¦ |
16:05-16:20 |
A004-12 |
The nonmagnetic field in the parent body of Tagish Lake |
‘D–Ø ›‰
|
•\Ž¦ |
16:20-16:35 |
A004-13 |
‘¾•½—m[ŠC‘ÍÏ•¨‚̊‹«ŠâÎŽ¥‹CFFORC}‚ð—˜—p‚µ‚½—¤Œ¹E¶•¨Œ¹¬•ª‚Ì•Ï“®‚Ì„’è |
ŽRè rŽk
|
•\Ž¦ |
16:35-16:50 |
A004-14 |
Ultra-fine scale magnetostratigraphy of Mn Crust by SQUID microscopy with spacial domain inversion |
¬“c Œ[–M
㓈 ³l
‰Pˆä ˜N
‚Ù‚© |
•\Ž¦ |
16:50-17:05 |
A004-15 |
–ó—nŠâ‚Ì•\–Ê‚©‚ç“à•”‚É‚©‚¯‚ẴeƒŠƒG–@‚É‚¨‚¯‚éU•‘‚̕ω» |
•ŸŠÔ _Ži
|
•\Ž¦ |
17:05-17:20 |
A004-16 |
‹ãBCz–K”V£“‡‰ÎŽR–¾Ž¡—nŠâ‚ÌŽ¥‹CŠâΊw“I“Á’¥‚Æ•¬‰ÎƒvƒƒZƒX |
âV“¡ •Žm
Îì ®l
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•\Ž¦ |