Matter
Name
Pigment Beauregard (PIG_0174_A_601), powder (grains inf. 160µm)
Family
mineral
Comments
also contain trace amount of Manganese and clay minerals (not detected by DRX)
Database
Experimentalists
Parent matter
Pigment Beauregard facies A (PIG_0174_A), hematite-rich vein
Level
from laboratory repository
Origins
natural terrestrial
Provider
Pigmenthothèque - EDYTEM
Provider reference code
Beauregard < 160 µm – PIG_0174_A_601 (2016-023)
Local reference code
PIG_0174_A_601_Beauregard-inf160
Body name
Earth
Terrain type
mineral surface
Place
Thoste, Côte d'Or , Bourgogne-Franche-Comté , France

Coordinates

System
WGS84
Position type
point
Geolocation
Point Latitude Longitude Altitude
#1 47.44768° 4.22644°
Comments
in heap
Preparation
sieved fraction
Method
crushed and sieved with a mesh of 160 µm
Storage condition
room temperature and conditions
Phase type
solid
Component type (group)
sedimentary rock (iron-sediment or ironstone)
Comments
Ferruginised crinoid-rich wackstone-packstone containing entirely ferruginised crinoid fragments (3mm) in a hematite-rich cement - Era: Mesozoic, lower Jurassic, Hettangien ferrugineux
Shape
very fine dark red-bordeaux powder
Texture
pulverulent
Type of porosity
particulate
Density
1.09 ± 0.15 g.cm3
Texture
compact
Grain density
1.09 ± 0.15 g.cm3
Grain sizes
Grains Size min Size max Size median Size width Size mass fraction Grain shape
#1 0.0 μm 160.0 μm 1.0 equant
Size distribution
possibly large fraction below 50-100 µm
Size method
sieving with mesh of 160 µm
Comments
density varies with the degree of settlement
Oxides
Formula SiO2 Al2O3 Fe2O3 MnO MgO CaO Na2O K2O TiO2 P2O5
Mass fraction (%) 8.51 2.48 75.94 2.82 0.07 1.54 0.015 0.32 0.1 0.46
Oxides comments
Contain Mn and Ca (4.36% in oxide) and small impurity of P, Ti, Na, K, Mg, (0.97% in oxides), fire loss: 5.66%
Number
4
Mode of mixing
heterogeneous mixing
Materials
  Name Arrangement Mass (g) Mass fraction Abundance comments
Hematite-goethite hematite and minor amount of goethite both in cement and as pseudomorphosis of bioclasts (crinoids and others) 0.917 91.7% of the crystalline phases
Quartz grains embeded in a ferric matrix (hematite + some goethite) 0.05 < 5%. Assumed mass fraction = cross section fraction in raw material. But possibly less if not crushed as original grains are larger (200-500µm) than sieve
Fluorite grains embeded in a ferric matrix (hematite + some goethite) 0.05 < 5%. Assumed mass fraction = cross section fraction in raw material
Baryte grains embeded in a ferric matrix (hematite + some goethite) 0.05 < 5%. Assumed mass fraction = cross section fraction in raw material