Determination of the Provenience of Majolica Pottery Found in the Caribbean Area Using Its Gamma-Ray Induced Thermoluminescence

1975 ◽  
Vol 40 (1) ◽  
pp. 71-82 ◽  
Author(s):  
J. Eduardo Vaz ◽  
José M. Cruxent

The gamma-ray induced thermoluminescence of specimens of majolica pottery of known origin, and of specimens of majolica of unknown origin collected in the Caribbean area was analyzed to determine if thermoluminescence could be used as an indicator of the provenience of pottery found in an archaeological context. The results of the measurements show that the shape of the gamma-ray induced thermoluminescence glow-curve of the clay matrix of majolica is specific to the geographic locality where the pottery was made, and that the provenience of specimens found archaeologically can be determined on the basis of their thermoluminescence glow-curves, when the curves obtained from the samples with known origins are used as references.

2018 ◽  
Author(s):  
N. J. Shivaramu ◽  
B. N. Lakshminarasappa ◽  
K. R. Nagabhushana ◽  
E. Coetsee ◽  
H. C. Swart

2015 ◽  
Vol 8 (1) ◽  
pp. 1-10 ◽  
Author(s):  
Raunak Kumar Tamrakar ◽  
Neha Tiwari ◽  
R.K. Kuraria ◽  
D.P. Bisen ◽  
Vikas Dubey ◽  
...  

1994 ◽  
Vol 47 (3) ◽  
pp. 189-192 ◽  
Author(s):  
Petr Vampola ◽  
František Kotlaba ◽  
Zdeněk Pouzar
Keyword(s):  

2021 ◽  
Vol 13 (10) ◽  
pp. 1939
Author(s):  
Tao Xian ◽  
Gaopeng Lu ◽  
Hongbo Zhang ◽  
Yongping Wang ◽  
Shaolin Xiong ◽  
...  

The thermal structure of the environmental atmosphere associated with Terrestrial Gamma-ray Flashes (TGFs) is investigated with the combined observations from several detectors (FERMI, RHESSI, and Insight-HXMT) and GNSS-RO (SAC-C, COSMIC, GRACE, TerraSAR-X, and MetOp-A). The geographic distributions of TGF-related tropopause altitude and climatology are similar. The regional TGF-related tropopause altitude in Africa and the Caribbean Sea is 0.1–0.4 km lower than the climatology, whereas that in Asia is 0.1–0.2 km higher. Most of the TGF-related tropopause altitudes are slightly higher than the climatology, while some of them have a slightly negative bias. The subtropical TGF-producing thunderstorms are warmer in the troposphere and have a colder and higher tropopause over land than the ocean. There is no significant land–ocean difference in the thermal structure for the tropical TGF-producing thunderstorms. The TGF-producing thunderstorms have a cold anomaly in the middle and upper troposphere and have stronger anomalies than the deep convection found in previous studies.


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