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Aqueous Alteration of Chondrites and Organic Matter 1
Thursday, August 1, 2024, 1:30 PM
Albert II Auditorium
Chairs:
Romy Hanna
Maizey Benner
Maizey Benner
1:30 PM
Gibson H. E.*
Daly L.
The Winchcombe Meteorite: The Woodmancote Stones and a New Lithology?
[#6102]
This study reports on a lithological analysis of a piece of the Winchcombe meteorite from a new site (Woodmancote) and is interpreted as a potential new lithology (I). This adds to the eight (A-H) identified from other sites along the strewn field.
This study reports on a lithological analysis of a piece of the Winchcombe meteorite from a new site (Woodmancote) and is interpreted as a potential new lithology (I). This adds to the eight (A-H) identified from other sites along the strewn field.
1:45 PM
Einsle J. F.*
Griffin S.
Floyd C.
Lehnert K. A.
Lee M. R.
Leveraging Uncertainty to Guide Lithographic Classification of the Cold Bokkeveld Carbonaceous Chondrite: A Data Driven Multiscale Correlative Study
[#6361]
An outstanding problem in understanding the aqueous alternation of C-complex derived meteorites is the lithographic classification of clasts in brecciated samples. We use a new approach to derive these classifications using machine learning.
An outstanding problem in understanding the aqueous alternation of C-complex derived meteorites is the lithographic classification of clasts in brecciated samples. We use a new approach to derive these classifications using machine learning.
2:00 PM
Findlay R.*
Franchi I. A.
Zolensky M. E.
Greenwood R. C.
Anand M.
et al.
Lithological Diversity of a C-Complex Asteroid Recorded in Lonewolf Nunataks 94101
[#6400]
Here we present an coordinated petrographical and O-isotope study of 19 lithologies from the Lonewolf Nunataks 94101 Antarctic CM2 chondrite.
Here we present an coordinated petrographical and O-isotope study of 19 lithologies from the Lonewolf Nunataks 94101 Antarctic CM2 chondrite.
2:15 PM
Cardon-Pilotaz P.*
Krot A. N.
Nagashima K.
Alevy E. G.
Dunn T. L.
Mineralogically Pristine, Metamorphosed and Metasomatically Altered Refractory Inclusions in CK3/CV3-4 Chondrite Breccia Camel Donga 003
[#6079]
We report on mineralogy and petrography of refractory inclusions in Camel Donga 003, a CK3/CV3-4 breccia. Refractory inclusions of CD003 have experienced various degrees of metamorphism, from pristine to extensively metamorphosed.
We report on mineralogy and petrography of refractory inclusions in Camel Donga 003, a CK3/CV3-4 breccia. Refractory inclusions of CD003 have experienced various degrees of metamorphism, from pristine to extensively metamorphosed.
2:30 PM
Lodders K.*
Mobile Elements in CI-Chondrites
[#6365]
Histograms of concentration frequency distributions can serve as quality controls and may provide insights on mobile element precipitation and redistribution during aqueous alteration on the CI-chondrite parent bodies and during meteorite storage.
Histograms of concentration frequency distributions can serve as quality controls and may provide insights on mobile element precipitation and redistribution during aqueous alteration on the CI-chondrite parent bodies and during meteorite storage.
2:45 PM
Daly L.*
Suttle M. D.
Lee M. R.
Bridges J.
Hicks L.
et al.
CM Carbonaceous Chondrites: Phase Heritage of Tochilinite-Cronstedtite Intergrowths Reveal a Carbonate Precursor
[#6307]
What were TCIs? / Texture suggests carbonate / Where did carbon go?
What were TCIs? / Texture suggests carbonate / Where did carbon go?
3:00 PM
Lee M. R.*
Almeida T.
The Thermal Stability of Tochilinite in CM Meteorites Measured by TEM Heating Experiments
[#6048]
At what temperature does tochilinite break down during heating of CM parent bodies?
At what temperature does tochilinite break down during heating of CM parent bodies?
3:15 PM
Benner M. C.*
Schrader D. L.
Zega T. J.
A Coordinated Analytical Investigation of Sulfide Minerals in Type 1 Chondrites as Analogues to Bennu and Ryugu
[#6199]
We investigate pyrrhotite and pentlandite minerals in Orgueil CI1.0 and Kolang CM 1.0 chondrites as analogues to Bennu and Ryugu. Thermodynamic conditions of alteration are constrained based on structure and composition.
We investigate pyrrhotite and pentlandite minerals in Orgueil CI1.0 and Kolang CM 1.0 chondrites as analogues to Bennu and Ryugu. Thermodynamic conditions of alteration are constrained based on structure and composition.
3:30 PM
Harrison C. S.*
King A. J.
Jones R. H.
Formation Conditions of Apatite and Mg-Phosphates in CI and CY Chondrites
[#6405]
We characterize phosphate grains within CI and CY carbonaceous chondrites. We find they contain rare Mg-phosphates and F-rich apatite, indicating the phosphates formed under similar fluid compositions on their respective parent bodies.
We characterize phosphate grains within CI and CY carbonaceous chondrites. We find they contain rare Mg-phosphates and F-rich apatite, indicating the phosphates formed under similar fluid compositions on their respective parent bodies.
3:45 PM
Ushikubo T.*
Tomioka N.
Yamaguchi A.
Isotopic and Mineralogical Study of Carbonates in Aguas Zarcas (CM2)
[#6082]
We present isotopic and mineralogical study of Ca-rich carbonates of the Aguas Zarcas (CM2) meteorite using SEM, SIMS, EPMA, and TEM.
We present isotopic and mineralogical study of Ca-rich carbonates of the Aguas Zarcas (CM2) meteorite using SEM, SIMS, EPMA, and TEM.
4:00 PM
Ong I. J.*
Barnes J. J.
Smith L. R.
Haenecour P.
Zega T. J.
et al.
Coordinated Microanalytical Study of Hydrothermal Alteration in the Winchcombe Meteorite
[#6252]
We are reporting the mineralogical and petrological work on carbonates within different petrological contexts to understand differences in formation conditions on the Winchcombe parent body.
We are reporting the mineralogical and petrological work on carbonates within different petrological contexts to understand differences in formation conditions on the Winchcombe parent body.
4:15 PM
Hanna R. D.*
Miller K. E.
Whittington A.
Bartels K.
Edey D. R.
et al.
Highly Porous Clast with Higher Aqueous Alteration and Carbonate Abundance in CM Murchison
[#6355]
We examine the relationships between porosity, aqueous alteration, and carbonate abundance in CM Murchison, with possible implications for the interpretation of Bennu's aqueous alteration history.
We examine the relationships between porosity, aqueous alteration, and carbonate abundance in CM Murchison, with possible implications for the interpretation of Bennu's aqueous alteration history.
4:30 PM
Bailey E.*
Telus M.
Lam P.
Webb S.
Fe XANES Analysis of Carbonates in CM Chondrites Reveals Varying Redox States During Aqueous Alteration
[#6464]
CM chondrites contain carbonate minerals that formed during progressive aqueous alteration. Synchrotron Fe XANES measurements of CM chondrites reveal a complex history of oxidation states preserved in individual calcite and dolomite grains.
CM chondrites contain carbonate minerals that formed during progressive aqueous alteration. Synchrotron Fe XANES measurements of CM chondrites reveal a complex history of oxidation states preserved in individual calcite and dolomite grains.
4:45 PM
Vacher L. G.*
Laize-Générat L.
Bonal L.
Flandinet L.
Poch O.
et al.
Search for Multiple Isotopic Carriers of Nitrogen in Type 2 Chondrites
[#6285]
We report here the bulk C and N elemental and isotopic compositions of a suite of CM chondrites. We try to identify the main N carriers using the IRMS technique. We also report the first bulk δ15N analysis for Asuka 12236 and Paris.
We report here the bulk C and N elemental and isotopic compositions of a suite of CM chondrites. We try to identify the main N carriers using the IRMS technique. We also report the first bulk δ15N analysis for Asuka 12236 and Paris.
*presenter