Marble analysis, 50.1321
Fragment of the statuette of a river god
White marble
Places of origin:
50.1321 and 50.1321 I: Marmara (Turkey)
50.1321 II: Marmara (Turkey) or Paros (Greece)
50.1321 III: Carrara (Italy)
Sample 50.1321 and 50.1321 I
Mineralogy: calcite
Texture: heteroblastic
Maximum grain size: 3.38 mm (50.1321); 1.63 mm (50.1321 I)
δ18OV-PDB: -0.36 ‰ (50.1321); -0.91 ‰ (50.1321 I)
δ13CV-PDB: 3.36 ‰ (50.1321); 3.31 ‰ (50.1321 I)
Cathodoluminescence color: blue-purple, mauve and brown (50.1321); brown-pink (50.1321 I)
Cathodoluminescence intensity: weak
Cathodoluminescence distribution: heterogeneous (50.1321); homogeneous (50.1321 I)
The isotopic signature, the MGS, the texture and the color of luminescence of this marble support Marmara as its origin.
Sample 50. 1321 II
Mineralogy: calcite
Texture: heteroblastic
Maximum grain size: 1.67 mm
δ18OV-PDB: -2.96 ‰
δ13CV-PDB: 2.52 ‰
Cathodoluminescence color: brown-pink
Cathodoluminescence intensity: weak
Cathodoluminescence distribution: homogeneous
The isotopic values are situated in the Paros and Marmara fields, two marbles with weak luminescence. It seems most probable that this statue was carved from a marble of Paros-Choriodaki, but we do not exclude an origin of Marmara.
Sample 50.1321 III
Mineralogy: calcite
Texture: homeoblastic
Maximum grain size: 0.53 mm
δ18OV-PDB: -1.92 ‰
δ13CV-PDB: 2.09 ‰
Cathodoluminescence color: orange and brown-orange
Cathodoluminescence intensity: intermediate
Cathodoluminescence distribution: heterogeneous
Stable isotopic signature fall in a zone where different source areas (i.e., overlap and the data are not conclusive. However the MGS, the texture and the orange color of luminescence support Carrara as its origin.
D. Decrouez & K. Ramseyer (1998, 2017)












