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Titlebook: Perspectives on Mind; Herbert R. Otto,James A. Tuedio Book 1988 D. Reidel Publishing Company, Dordrecht, Holland 1988 Edmund Husserl.anima

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樓主: 呻吟
11#
發(fā)表于 2025-3-23 09:43:46 | 只看該作者
第4樓
12#
發(fā)表于 2025-3-23 14:28:15 | 只看該作者
13#
發(fā)表于 2025-3-23 21:45:49 | 只看該作者
,Arbeitsformen des Gruppengespr?chs, das ?Referat mit anschlie?ender Aussprache?, wobei der Unterschied zwischen Vortrag und Referat darin zu liegen scheint, da? man sich beim ersteren auf eine L?nge von etwa einer bis zu zweieinhalb Stunden einstellt, w?hrend man beim letzteren mit einer halben bis dreiviertel Stunde zufrieden ist..
14#
發(fā)表于 2025-3-24 01:06:25 | 只看該作者
15#
發(fā)表于 2025-3-24 03:44:23 | 只看該作者
SurgicalManagement of Elderly Patientsination, leading to a poor alignment between strategic management and operational business processes execution. Researchers and professionals of information systems have recognized that business processes are the key for identifying the user needs for developing the software that supports those need
16#
發(fā)表于 2025-3-24 07:46:58 | 只看該作者
17#
發(fā)表于 2025-3-24 14:08:52 | 只看該作者
Artur Maier,Carolin Mügge,Dirk TischlerPity the poor reader! A succession of unduly long articles is bad enough, but if each is followed by a plethora of references the effect is positively daunting. Even the reader who is impressed by the length of a list may question the author‘s discrimination. Were all those references needed? Were t
18#
發(fā)表于 2025-3-24 18:29:12 | 只看該作者
D. D. Joseph such direct extension exists however, for dynamics. Inertia binor is used to obtain the dual momentum, from which the dual equations of motion are derived. This derivation raises the dual dynamic equations to six dimensions, and in fact, it does not act on the dual vector as a whole, but rather on
19#
發(fā)表于 2025-3-24 19:58:03 | 只看該作者
20#
發(fā)表于 2025-3-25 03:04:21 | 只看該作者
Heather Grabbe and the oceans when the surface temperature of the sea falls below, approximately, -2°C. Dynamic environmental conditions introduce significant variability into this layer over many length scales of interest to the underwater acoustian (from millimetres to kilometres). Arctic pack ice, for example,
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