• Tidak ada hasil yang ditemukan

A review of the archaeological analogue (1)

N/A
N/A
Protected

Academic year: 2018

Membagikan "A review of the archaeological analogue (1)"

Copied!
10
0
0

Teks penuh

Loading

Gambar

Fig. 1. (Left) Place of the archaeological analogues in the long-term corrosion behaviour prediction phenomenological modelling approach, (right) specific methodologyadopted in France for archaeological analogues studies.
Table 1
Fig. 2. (Left) On field measurements on the archaeological site of Glinet. Map of the archaeological site
Fig. 4. EXAFS data obtained on iron containing phases present on archaeological samples; (left) k�chi(k) EXAFS signal and (right) FT(k.chi(k)) Fourier Transform [35].
+4

Referensi

Dokumen terkait

Field research involving core drilling methods applied in the area of Sungai Batu Archaeological Complex with the main purpose of obtaining primary data related

EFFECTS OF FILM FORMATION OF H2S GAS ON CARBON STEEL CORROSION Figure 2 presents the simulated corrosion rate of carbon steel due to the presence of H 2 S in CO 2..

TLOKWA HISTORY: REPORT ON AN ARCHAEOLOGICAL SURVEY OF STONE-WALLED SITES IN THE NORTH-EASTERN FREE STATE* J.DREYER Department of Amhropology, University of the Free State,

Precisely because the founding condition of the national is the transnational and not an original, native corpus of texts as in historicism’s organic conception of culture, we may say

Considering the previous experiences of SARS-CoV and other viral diseases, some potential therapeutic agents such as hydroxychloroquine, interferons, nucleoside analogues, remdesivir,

D mm= 1.30d 5 Length of mixing chamber The length of the mixing chamber L was deter- mined from equation 6 L= 1.50d 6 Number of holes The number of holes on the burner was estimated

No dif- ferences between these additional sequences and that deter- mined from patient 1 were found in the 16S rRNA gene leader region, the 23S rRNA gene region containing the

This paper summarises the geological evolution as: building blocks formed during Proterozoic and Palaeozoic times; development of a Mesozoic mid-latitude passive margin on the eastern