Titlebook: STRATI 2013; First International Rogério Rocha,Jo?o Pais,Stanley Finney Conference proceedings 2014 Springer International Publishing Swit

監(jiān)禁

Michaela Berneckeris human freedom (.); if there is human freedom, then there exists a set of true propositions about the actual world (∑α′) describing the physical substituents of freedom; these same substituents imply the possibility of natural evil (.). Therefore, the existence of God implies the possibility of th

痛打

arcane

Jaume Dinarès-Turell,Aitor Payros,Simonetta Monechi,Xabier Orue-Etxebarria,Silvia Ortiz,Estibaliz Apis human freedom (.); if there is human freedom, then there exists a set of true propositions about the actual world (∑α′) describing the physical substituents of freedom; these same substituents imply the possibility of natural evil (.). Therefore, the existence of God implies the possibility of th

不能仁慈

harmony

Sequence Stratigraphy of Continental Rift Basins II: An Example from the Brazilian Cretaceous Rec?nc already more advanced rifting phase. When the rifting ends, the accommodation rate decreases, the sedimentation regime is progradational, and the rift basin is filled with fluvial, deltaic, and aeolian facies.

擔(dān)心

The Triassic Timescale 2013s the following calibrations: base of Triassic?~252?Ma, base Olenekian?~251?Ma, base Anisian?~247?Ma, base Ladinian?~242?Ma, base Norian?~221?Ma, and base Jurassic?~201?Ma. Triassic magnetostratigraphy is a series of multichrons at best, and needs vast improvement to make a serious contribution to t

defeatist

Bio- and Lithostratigraphic Markers of the Mid-Pennsylvanian Event and Their Application to Detailednt of . was found at the top of the Domodedovo Formation in the Kasimov quarry. The occurrence of erosion surfaces increases into the upper Domodedovo Formation and Peski Formation. The change in sedimentation is marked by an input of siliciclastic material, which allows the lower boundary of the Vo

Neuralgia

The Alano Section: The Candidate GSSP for the Priabonian Stagerominent crystal tuff layer, the Tiziano bed, located at the 63.57?m level in the Alano section. Following the publication of this proposal, a unanimous consensus on the Alano section as the GSSP of the Priabonian (i.e., Gradstein et al. .; Wade et al. .) has been reached during an ad hoc workshop h

雄辯

昏迷狀態(tài)

In Search of the Bartonian (Middle Eocene) GSSP (II): Preliminary Results from the Oyambre Section ( Acebosa Formation. A denser magnetostratigraphic and biostratigraphic sampling is required in the upper part of this unit in order to accurately identify Chron C19n and to establish the sequence of events across the Lutetian–Bartonian transition.