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  • T1. Geochronology
  • T1.1 – Geochronology and Thermochronology

PANOPLY (Plateforme Analytique Géosciences Paris Saclay)

Located on the “Plateau de Saclay”, PANOPLY offers to the academic and industrial scientific communities an array of high tech resources in the fields of Earth, Climate, and Environmental Sciences.
This integrated platform, provides a wide array of high quality services (ranging from routine analyses to full scientific collaboration) and brings together expert research teams operating in a highly professional environment. It opens access to cutting edge technology in the fields of geochemistry and mineralogy.

PANOPLY is organised into four principal centres of expertise - mineralogical analysis, elemental analysis, isotopic analysis and radioactivity measurements - each of which encompasses a package of technological platforms that have been brought together under the supports of PANOPLY in order to optimise the provision of complementary services.

News

A look back at the RéGEF Stable Isotopes Days days from September 26 to 27, 2024
Installation of a GC-FID on the organic geochemistry platform
A 2000-year temperature reconstruction on the East Antarctic plateau from argon–nitrogen and water stable isotopes in the Aurora Basin North ice core
The ST22 chronology for the Skytrain Ice Rise ice core – Part 2: An age model to the last interglacial and disturbed deep stratigraphy
Differences in carbonate chemistry up-regulation of long-lived reef-building corals

Analyses by sample type

Water
Ice
Sediments and soils
Rocks and minerals
Carbonates
Wood and organic matter
Gas

T1.1 – Geochronology and Thermochronology

  • Dating of continental and oceanic geological archives [K-Ar, 40Ar/39Ar, U/Th and 14C dating]

  • Calibration of timescales – Standardisation of timescales [K-Ar. 40Ar/39Ar,U/Th and14C dating,Archaeomagnetic dating, Magnetostratigraphy]

  • 14C Calibration. Marine and lacustrine reservoir ages [14C,U/Th,Palaeomagnetism]

  • Dynamics of volcanic systems [K-Ar and40Ar/39Ar dating]

  • Formation of mountain ranges [Low temperature thermochronology: (U-Th)/He and apatite and/or zircon fission track analysis-K-Ar and40Ar/39Ar dating]

  • Filling and inversion of sedimentary basins [Low-temperature thermochronology: (U-Th)/He and apatite and/or zircon fission track analysis-K-Ar and40Ar/39Ar dating]

  • Evolution of passive margins [Low temperature thermochronology: (U-Th)/He and apatite and/or zircon fission track analysis -K-Ar and40Ar/39Ar dating]

  • Next

Scientific themes

  • Geochronology

  • Geochemistry and transfer of water and contaminants in the environment

  • Palaeoclimatology and palaeoceanography

  • Sedimentary transfers, diagenesis and resources

 

Isotopic analyses

H He
Li Be B C N O F Ne
Na Mg Al Si P S Cl Ar
K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Kr
Rb Sr Y Zr Nb Mo Tc Ru Rh Pd Ag Cd In Sn Sb Te I Xe
Cs Ba La Hf Ta W Re Os Ir Pt Au Hg Tl Pb Bi Po At Rn
Fr Ra Ac Ku Ha
   
   
   
Ce Pr Nd Pm Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Th Pa U Np Pu Am Cm Bk Cf Es Fm Md No Lw

Type of analysis

- Mineral

- Elemental

- Isotopic

- Molecular

- Radioactivity

Elemental analyses

 H                                  He
 Li  Be                      B  C  N  O  F  Ne
 Na  Mg                      Al  Si  P  S  Cl  Ar
 K  Ca  Sc  Ti  V Cr  Mn  Fe  Co  Ni  Cu  Zn  Ga  Ge As  Se  Br  Kr
 Rb  Sr  Y  Zr Nb  Mo  Tc  Ru  Rh  Pd Ag Cd  In  Sn  Sb  Te  I  Xe
 Cs  Ba  La  Hf  Ta  W  Re  Os  Ir  Pt  Au  Hg  Tl  Pb  Bi  Po  At  Rn
 Fr  Ra  Ac  Ku  Ha                          
   
   
   
                             
                                   
        Ce Pr Nd Pm Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
         Th  Pa  U  Np  Pu  Am  Cm  Bk  Cf  Es  Fm  Md  No  Lw

 

 

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