Descriptif ED1112-MTP - Historique des versions

Laure le 16 décembre 2011 à 09:54

Laure — Fri, 16 Dec 2011 09:54:04 GMT

← Version précédente		Version du 16 décembre 2011 à 09:54
Ligne 9 :		Ligne 9 :


-	Les intervenants sont :	+	Les intervenants sont :<br>
-	Bernard Bourdon (ENS Lyon) will present constrains on Earth formation and differentiation from geochemistry	+	Bernard Bourdon (ENS Lyon) will present constrains on Earth formation and differentiation from geochemistry<br>
-	Razvan Caracas (ENS Lyon) will use theoretical mineral physics to gain insight into core composition	+	Razvan Caracas (ENS Lyon) will use theoretical mineral physics to gain insight into core composition<br>
-	Stephane Labrosse (ENS Lyon) will develop core cooling models in relation with mantle structure and dynmaics	+	Stephane Labrosse (ENS Lyon) will develop core cooling models in relation with mantle structure and dynmaics<br>
-	Mike Walter (U. Bristol) will apply experimental petrology and mineral physics to unveil the composition of the mantle	+	Mike Walter (U. Bristol) will apply experimental petrology and mineral physics to unveil the composition of the mantle<br>
-	Lidunka Vocadlo (UCL London) will depict core structure from theoretical mineral physics	+	Lidunka Vocadlo (UCL London) will depict core structure from theoretical mineral physics<br>
-	Ana Ferreira (UEA Norwich) will apply global seismology to the study on mantle structure and heterogeneity	+	Ana Ferreira (UEA Norwich) will apply global seismology to the study on mantle structure and heterogeneity<br>
-	Julien Siebert (UPMC/IPGP) will present a new model of core formation based on experimental and theoretical physics	+	Julien Siebert (UPMC/IPGP) will present a new model of core formation based on experimental and theoretical physics<br>

-	James Badro (IPGP) and Julien Siebert (UPMC/IPGP) will present a 1-day graduate course in thermodynamics, experimental petrology, and mineral physics	+	James Badro (IPGP) and Julien Siebert (UPMC/IPGP) will present a 1-day graduate course in thermodynamics, experimental petrology, and mineral physics<br>

Laure le 16 décembre 2011 à 09:53

Laure — Fri, 16 Dec 2011 09:53:34 GMT

← Version précédente		Version du 16 décembre 2011 à 09:53
Ligne 5 :		Ligne 5 :
	'''Investigating the Deep Earth: Observation, Experiments, and Models'''		'''Investigating the Deep Earth: Observation, Experiments, and Models'''

-	''The '''deep Earth''' is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology).<br> In order to '''better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments''', and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard:<br> '''Francis Birch''' has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, '''Ted Ringwood '''has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br>Last,''' the 410, 550, and 660 seismic discontinuities''' in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br> The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to '''highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics)''', and to present the models that emerge from their interaction.	+	''The '''deep Earth''' is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology).<br> In order to '''better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments''', and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard:<br> '''Francis Birch''' has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, '''Ted Ringwood '''has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br>Last,''' the 410, 550, and 660 seismic discontinuities''' in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br> The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to '''highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics)''', and to present the lastest models that emerge from their interaction.
	<br>''		<br>''


	Les intervenants sont :		Les intervenants sont :
-	Bernard Bourdon (ENS Lyon)~~<br>~~	+	Bernard Bourdon (ENS Lyon) will present constrains on Earth formation and differentiation from geochemistry
-	Razvan Caracas (ENS Lyon)~~<br>~~	+	Razvan Caracas (ENS Lyon) will use theoretical mineral physics to gain insight into core composition
-	Stephane Labrosse (ENS Lyon)~~<br>~~	+	Stephane Labrosse (ENS Lyon) will develop core cooling models in relation with mantle structure and dynmaics
-	Mike Walter (U. Bristol)~~<br>~~	+	Mike Walter (U. Bristol) will apply experimental petrology and mineral physics to unveil the composition of the mantle
-	Lidunka Vocadlo (UCL London)~~<br>~~	+	Lidunka Vocadlo (UCL London) will depict core structure from theoretical mineral physics
-	Ana Ferreira (UEA Norwich)~~<br>~~	+	Ana Ferreira (UEA Norwich) will apply global seismology to the study on mantle structure and heterogeneity
-	Julien Siebert (UPMC/IPGP)~~<br>~~	+	Julien Siebert (UPMC/IPGP) will present a new model of core formation based on experimental and theoretical physics
-	~~James Badro (IPGP)<br>~~	+

		+	James Badro (IPGP) and Julien Siebert (UPMC/IPGP) will present a 1-day graduate course in thermodynamics, experimental petrology, and mineral physics

Laure le 14 décembre 2011 à 22:04

Laure — Wed, 14 Dec 2011 22:04:45 GMT

← Version précédente		Version du 14 décembre 2011 à 22:04
Ligne 1 :		Ligne 1 :
-	''Dates: 9 Mai, 14 et 15 Mai 2012; Lieu : Salle outremer, IPGP, Cuvier~~.''~~	+	Dates: 9 Mai, 14 et 15 Mai 2012; Lieu : Salle outremer, IPGP, Cuvier

	Ce module est organisé sous la forme de jours de conférences_cours.		Ce module est organisé sous la forme de jours de conférences_cours.

Laure le 14 décembre 2011 à 22:04

Laure — Wed, 14 Dec 2011 22:04:33 GMT

← Version précédente		Version du 14 décembre 2011 à 22:04
Ligne 5 :		Ligne 5 :
	'''Investigating the Deep Earth: Observation, Experiments, and Models'''		'''Investigating the Deep Earth: Observation, Experiments, and Models'''

-	The '''deep Earth''' is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology).<br> In order to '''better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments''', and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard:<br> '''Francis Birch''' has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, '''Ted Ringwood '''has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br>Last,''' the 410, 550, and 660 seismic discontinuities''' in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br> The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to '''highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics)''', and to present the models that emerge from their interaction.	+	''The '''deep Earth''' is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology).<br> In order to '''better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments''', and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard:<br> '''Francis Birch''' has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, '''Ted Ringwood '''has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br>Last,''' the 410, 550, and 660 seismic discontinuities''' in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br> The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to '''highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics)''', and to present the models that emerge from their interaction.
-	<br>	+	<br>''

Laure le 14 décembre 2011 à 22:04

Laure — Wed, 14 Dec 2011 22:04:16 GMT

← Version précédente		Version du 14 décembre 2011 à 22:04
Ligne 1 :		Ligne 1 :
-	""Dates: 9 Mai, 14 et 15 Mai 2012; Lieu : Salle outremer, IPGP, Cuvier.	+	''Dates: 9 Mai, 14 et 15 Mai 2012; Lieu : Salle outremer, IPGP, Cuvier.''

	Ce module est organisé sous la forme de jours de conférences_cours.		Ce module est organisé sous la forme de jours de conférences_cours.

Laure le 14 décembre 2011 à 22:03

Laure — Wed, 14 Dec 2011 22:03:42 GMT

← Version précédente		Version du 14 décembre 2011 à 22:03
Ligne 5 :		Ligne 5 :
	'''Investigating the Deep Earth: Observation, Experiments, and Models'''		'''Investigating the Deep Earth: Observation, Experiments, and Models'''

-	The deep Earth is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology).<br> In order to better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments, and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard:<br> Francis Birch has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, Ted Ringwood has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br> Last, the 410, 550, and 660 seismic discontinuities in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br> The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics), and to present the models that emerge from their interaction.	+	The '''deep Earth''' is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology).<br> In order to '''better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments''', and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard:<br> '''Francis Birch''' has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, '''Ted Ringwood '''has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br>Last,''' the 410, 550, and 660 seismic discontinuities''' in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br> The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to '''highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics)''', and to present the models that emerge from their interaction.
	<br>		<br>

Laure le 14 décembre 2011 à 22:02

Laure — Wed, 14 Dec 2011 22:02:05 GMT

← Version précédente		Version du 14 décembre 2011 à 22:02
Ligne 1 :		Ligne 1 :
-	~~Encours~~	+	""Dates: 9 Mai, 14 et 15 Mai 2012; Lieu : Salle outremer, IPGP, Cuvier.
-		+
-	Dates ~~prévues~~ 14 et 15 Mai, Salle outremer, IPGP, Cuvier.	+

	Ce module est organisé sous la forme de jours de conférences_cours.		Ce module est organisé sous la forme de jours de conférences_cours.
		+
		+	'''Investigating the Deep Earth: Observation, Experiments, and Models'''
		+
		+	The deep Earth is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology).<br> In order to better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments, and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard:<br> Francis Birch has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, Ted Ringwood has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br> Last, the 410, 550, and 660 seismic discontinuities in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br> The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics), and to present the models that emerge from their interaction.
		+	<br>


Ligne 16 :		Ligne 19 :
	James Badro (IPGP)<br>		James Badro (IPGP)<br>

-	~~Investigating the Deep Earth: Observation, Experiments, and Models~~
-
-	The deep Earth is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology). In order to better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments, and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard: Francis Birch has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, Ted Ringwood has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br> Last, the 410, 550, and 660 seismic discontinuities in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br>The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics), and to present the models that emerge from their interaction.
-	~~<br>~~

Laure le 14 décembre 2011 à 21:59

Laure — Wed, 14 Dec 2011 21:59:40 GMT

← Version précédente		Version du 14 décembre 2011 à 21:59
Ligne 18 :		Ligne 18 :
	Investigating the Deep Earth: Observation, Experiments, and Models		Investigating the Deep Earth: Observation, Experiments, and Models

-	The deep Earth is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology). In order to better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments, and carry out what looks like a real "forensics" investigation. We can give a few examples of some seminal achievements in this regard: Francis Birch has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. Similarly, Ted Ringwood has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab. Last, the 410, 550, and 660 seismic discontinuities in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics), and to present the models that emerge from their interaction.	+	The deep Earth is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology). In order to better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments, and carry out what looks like a real "forensics" investigation.<br> We can give a few examples of some seminal achievements in this regard: Francis Birch has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. <br>Similarly, Ted Ringwood has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab.<br> Last, the 410, 550, and 660 seismic discontinuities in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. <br>The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics), and to present the models that emerge from their interaction.
-		+	<br>

Laure le 14 décembre 2011 à 21:52

Laure — Wed, 14 Dec 2011 21:52:49 GMT

← Version précédente		Version du 14 décembre 2011 à 21:52
Ligne 16 :		Ligne 16 :
	James Badro (IPGP)<br>		James Badro (IPGP)<br>

		+	Investigating the Deep Earth: Observation, Experiments, and Models
		+
		+	The deep Earth is not physically accessible, but it is however the object of intense studies by remote sensing (seismology, geoid, magnetism) and has left a measurable imprint on the shallow Earth (geochemistry, petrology). In order to better understand the structure, composition, and evolution of the deep Earth, and to propose models of composition, formation and evolution, we need to compare the observations with laboratory-based experiments, and carry out what looks like a real "forensics" investigation. We can give a few examples of some seminal achievements in this regard: Francis Birch has shown 50 years ago that the core is necessarily lighter than pure iron. He achieved this by comparing seismic observation of velocity-density in the core with lab-based experiments on pure iron. Similarly, Ted Ringwood has proposed that the mantle was composed of a synthetic rock called pyrolite, a mixture of olivine and pyroxenes. This again was obtained by linking the composition of MORB and mantle xenoliths to high-pressure phase equilibrium studies in the lab. Last, the 410, 550, and 660 seismic discontinuities in the mantle were linked, one after the other, to physical changes in mantle minerals, namely olivine, at high pressure and high temperature. The objective of this 3-day (1 day graduate, 2 day postgraduate) course is to highlight the different domains of investigation of the deep Earth (Seismology, Geochemistry, Experimental Petrology, Mineral Physics, Geodynamics), and to present the models that emerge from their interaction.

Laure le 1 décembre 2011 à 04:19

Laure — Thu, 01 Dec 2011 04:19:40 GMT

← Version précédente		Version du 1 décembre 2011 à 04:19
Ligne 1 :		Ligne 1 :
	Encours		Encours
		+
		+	Dates prévues 14 et 15 Mai, Salle outremer, IPGP, Cuvier.
		+
		+	Ce module est organisé sous la forme de jours de conférences_cours.
		+
		+
		+	Les intervenants sont :
		+	Bernard Bourdon (ENS Lyon)<br>
		+	Razvan Caracas (ENS Lyon)<br>
		+	Stephane Labrosse (ENS Lyon)<br>
		+	Mike Walter (U. Bristol)<br>
		+	Lidunka Vocadlo (UCL London)<br>
		+	Ana Ferreira (UEA Norwich)<br>
		+	Julien Siebert (UPMC/IPGP)<br>
		+	James Badro (IPGP)<br>
		+
		+
		+
		+
	<br>		<br>
	'''Pour les doctorants autres que les doctorants ED109''': Merci de vous inscrire en indiquant votre nom, prénom, mail et le n° de votre École Doctorale		'''Pour les doctorants autres que les doctorants ED109''': Merci de vous inscrire en indiquant votre nom, prénom, mail et le n° de votre École Doctorale
	à scol-ed@ipgp.fr		à scol-ed@ipgp.fr
	<br>		<br>