Log in

Relevant bibliographies by topics / Geochemistry – Tunisia / Journal articles

To see the other types of publications on this topic, follow the link: Geochemistry – Tunisia.

Journal articles on the topic 'Geochemistry – Tunisia'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the top 50 journal articles for your research on the topic 'Geochemistry – Tunisia.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Browse journal articles on a wide variety of disciplines and organise your bibliography correctly.

1

Trabelsi, Rim, Kamel Abid, and Kamel Zouari. "Geochemistry processes of the Djeffara palaeogroundwater (Southeastern Tunisia)." Quaternary International 257 (April 2012): 43–55. http://dx.doi.org/10.1016/j.quaint.2011.10.029.

Full text

APA, Harvard, Vancouver, ISO, and other styles

2

Garali, Amor B., Mohamed Ouakad, and Moncef Gueddari. "Geochemistry of episodic sedimentation in Bizerte Lagoon, northern Tunisia." Lakes & Reservoirs: Research & Management 15, no. 3 (September 16, 2010): 273–82. http://dx.doi.org/10.1111/j.1440-1770.2010.00433.x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

3

Helali, Mohamed Amine, Walid Oueslati, Noureddine Zaaboub, Ayed Added, and Saadi Abdeljaouad. "Geochemistry of marine sediments in the Mejerda River delta, Tunisia." Chemical Speciation & Bioavailability 25, no. 4 (January 2013): 247–57. http://dx.doi.org/10.3184/095422913x13840098160825.

Full text

APA, Harvard, Vancouver, ISO, and other styles

4

Montoroi, Jean-Pierre, Olivier Grünberger, and Slah Nasri. "Groundwater geochemistry of a small reservoir catchment in Central Tunisia." Applied Geochemistry 17, no. 8 (August 2002): 1047–60. http://dx.doi.org/10.1016/s0883-2927(02)00076-8.

Full text

APA, Harvard, Vancouver, ISO, and other styles

5

Dhia, Hamed Ben. "Thermal regime and hydrodynamics in Tunisia and Algeria." GEOPHYSICS 56, no. 7 (July 1991): 1093–102. http://dx.doi.org/10.1190/1.1443121.

Full text

Abstract:

The thermal regime of Algeria and Tunisia and its relation to hydrodynamics is studied by means of available geological and geothermal, and petroleum data. Heat flow densities in the area range from [Formula: see text] to [Formula: see text]. Several Paleozoic to Tertiary aquifers have been identified, together with potential recharge and discharge areas. The area is a transition zone between the African and European plates. The more tectonically active northern Alpine domain does not exhibit an obvious geothermal trend, and high heat flow anomalies that occur there may be related to structure rather than hydrodynamics. The more stable southern Saharan tectonic domain, with background heat flow of approximately [Formula: see text], exhibits anomalous zones correlated to the hydrodynamic regime with low values in recharge areas (Algerian Tinrhert and High Plateaux) and values in discharge areas (Tunisian Jeffara and Algerian Tademait). The hydrodynamic perturbation to the normal heat flow is estimated to be as great as [Formula: see text] in recharge and discharge zones.

APA, Harvard, Vancouver, ISO, and other styles

6

Garnit, Hechmi, Salah Bouhlel, and Ian Jarvis. "Geochemistry and depositional environments of Paleocene–Eocene phosphorites: Metlaoui Group, Tunisia." Journal of African Earth Sciences 134 (October 2017): 704–36. http://dx.doi.org/10.1016/j.jafrearsci.2017.07.021.

Full text

APA, Harvard, Vancouver, ISO, and other styles

7

Ben Garali, Amor, Mohamed Ouakad, and Moncef Gueddari. "Geochemistry of Bizerte lagoon affluent water, Northern Tunisia: principal component analysis." Arabian Journal of Geosciences 4, no. 3-4 (March 16, 2010): 475–81. http://dx.doi.org/10.1007/s12517-010-0128-z.

Full text

APA, Harvard, Vancouver, ISO, and other styles

8

Tlil, Haifa, Radhia Souissi, Fouad Souissi, Pierfranco Lattanzi, Francesca Podda, Sara Concas, Carla Ardau, and Rosa Cidu. "Environmental mineralogy and geochemistry of Pb–Zn mine wastes, Northern Tunisia." Rendiconti Lincei 28, no. 1 (December 9, 2016): 133–41. http://dx.doi.org/10.1007/s12210-016-0585-8.

Full text

APA, Harvard, Vancouver, ISO, and other styles

9

Garnit, Hechmi, Dennis Kraemer, Salah Bouhlel, Mariano Davoli, and Donatella Barca. "Manganese ores in Tunisia: Genetic constraints from trace element geochemistry and mineralogy." Ore Geology Reviews 120 (May 2020): 103451. http://dx.doi.org/10.1016/j.oregeorev.2020.103451.

Full text

APA, Harvard, Vancouver, ISO, and other styles

10

Houatmia, Faten, Sami Khomsi, Ammar Malayah, Mouna Andolssi, and Mourad Bedir. "Neogene aquifer: geochemistry and structuring in the Sidi Saad basin, central Tunisia." Arabian Journal of Geosciences 8, no. 6 (May 24, 2014): 4221–38. http://dx.doi.org/10.1007/s12517-014-1433-8.

Full text

APA, Harvard, Vancouver, ISO, and other styles

11

Ounissi, Chedlia, Salah Mahmoudi, Luca Valentini, Ali Bennour, Enrico Garbin, Gilberto Artioli, and Mabrouk Montacer. "Potential use of Kebilian clay reserves (southern Tunisia) for the production of geopolymer materials." Clay Minerals 55, no. 2 (May 6, 2020): 101–11. http://dx.doi.org/10.1180/clm.2020.14.

Full text

Abstract:

AbstractThe aim of this study was to help drive the Tunisian construction industry towards a more sustainable approach given the existence of abundant local raw material deposits that could be exploited for the production of low-CO2 binders. Various clay sediments from the Kebili region (southern Tunisia) were characterized by chemical analysis, X-ray diffraction, thermal analysis and geotechnical tests to determine their suitability for the preparation of geopolymer binders. The clays consist of illite and kaolinite with other accessory minerals. To test the possibility of using these materials as precursors for the production of low-CO2 and low-cost geopolymers, the raw samples were calcined and activated by addition of solid sodium silicate. Compressive strength tests performed on four alkali-activated clays show that promising mechanical performance may be achieved, with mechanical strength values as high as 25 MPa after 7 days, depending on the clay composition. The mechanical strength is related to the SiO2:Al2O3 and Al2O3:(NaO2 + K2O) ratios. Careful selection of the raw materials is, therefore, an essential step in the exploitation of clay deposits to be used for the production of ecological materials such as geopolymers.

APA, Harvard, Vancouver, ISO, and other styles

12

Belayouni, Habib, Maurice Slansky, and Jean Trichet. "A study of the organic matter in Tunisian phosphates series: Relevance to phosphorite genesis in the Gafsa Basin (Tunisia)." Organic Geochemistry 15, no. 1 (January 1990): 47–72. http://dx.doi.org/10.1016/0146-6380(90)90184-2.

Full text

APA, Harvard, Vancouver, ISO, and other styles

13

Jemmali, Nejib, Fouad Souissi, Emmanuel John M. Carranza, and Mohsen Henchiri. "Geochemistry of Triassic Carbonates: Exploration Guide to Pb-Zn Mineralization in North Tunisia." Resource Geology 66, no. 4 (September 12, 2016): 335–50. http://dx.doi.org/10.1111/rge.12104.

Full text

APA, Harvard, Vancouver, ISO, and other styles

14

Abid, Kamel, Kamel Zouari, Marek Dulinski, Najiba Chkir, and Brahim Abidi. "Hydrologic and geologic factors controlling groundwater geochemistry in the Turonian aquifer (southern Tunisia)." Hydrogeology Journal 19, no. 2 (November 11, 2010): 415–27. http://dx.doi.org/10.1007/s10040-010-0668-z.

Full text

APA, Harvard, Vancouver, ISO, and other styles

15

Essefi, Elhoucine. "Geochemistry and mineralogy of the sebkha Oum El Khialate evaporites mixtures, southeastern Tunisia." Resource Geology 71, no. 3 (March 9, 2021): 242–49. http://dx.doi.org/10.1111/rge.12264.

Full text

APA, Harvard, Vancouver, ISO, and other styles

16

GALFATI, I., A. B^|^Eacute;JI SASSI, A. ZA^|^Iuml;ER, J. L. BOUCHARDON, E. BILAL, J. L. JORON, and S. SASSI. "Geochemistry and mineralogy of Paleocene-Eocene Oum El Khecheb phosphorites (Gafsa-Metlaoui Basin) Tunisia." GEOCHEMICAL JOURNAL 44, no. 3 (2010): 189–210. http://dx.doi.org/10.2343/geochemj.1.0062.

Full text

APA, Harvard, Vancouver, ISO, and other styles

17

Laribi, S., J. M. Fleureau, and N. Kbir-Ariguib. "Filtration and standardized properties of Jebel Om El Khecheb clay (Tunisia) and Wyoming bentonite." Clay Minerals 42, no. 3 (September 2007): 319–28. http://dx.doi.org/10.1180/claymin.2007.042.3.05.

Full text

Abstract:

AbstractThe rheological and filtration properties of a Tunisian clay are presented and compared with those of Wyoming bentonite. The study was part of an evauation of Tunisian mining resources in general, and of the bentonitic deposits in particular. Qualitatively, the two clays exhibit the same rheological and filtration behaviour but quantitatively the properties of purified Wyoming bentonite are distinctly better at the same concentration. The difference can be related to the mineralogical structure and the presence of 13% illite in the Tunisian clay. Standard tests show that the rheological behaviour of the purified Tunisian clay is close to that of the raw Wyoming bentonite and conform to the American Petroluem Institute (A.P.I.) standards for medium-depth drilling formulations.

APA, Harvard, Vancouver, ISO, and other styles

18

Letaïef, S., B. Casal, N. Kbir-ariguib, M. Trabelsi–Ayadi, and E. Ruiz-hitzky. "Fe-rich smectites from Gafsa (Tunisia): characterization and pillaring behaviour." Clay Minerals 37, no. 3 (September 2002): 517–29. http://dx.doi.org/10.1180/0009855023730050.

Full text

Abstract:

AbstractThree raw samples of Fe-rich smectites from Gafsa (Jebels Shemsi and Hammadi, Tunisia) have been characterized by different techniques which indicate that they contain (15 – 20%) illite, probably interstratified and to a lesser extent they also contain kaolinite, calcite, quartz and Fe oxides. These samples present a relatively high Fe content (∼9%) in the <2 μm fraction. From EPR and Mössbauer spectroscopy it is deduced that Fe is mainly present as Fe(III) in the octahedral environment of smectites and also in Fe-oxyhydroxides associated with the clays. Aluminium-pillared clays have been prepared from the Na+-purified samples, and their thermal stability and acidity have been studied.

APA, Harvard, Vancouver, ISO, and other styles

19

Affouri, Hassene, Mabrouk Montacer, and Jean-Robert Disnar. "Organic Geochemistry of the Cenomanian-Turonian Bahloul Formation Petroleum Source Rock, Central and Northern Tunisia." Resource Geology 63, no. 3 (June 21, 2013): 262–87. http://dx.doi.org/10.1111/rge.12008.

Full text

APA, Harvard, Vancouver, ISO, and other styles

20

Zidi, Manel, Abderrazak El Albani, and Jamel Touir. "Abiod Formation in Boukhil section (Jebel M'rhila, Central Tunisia): Facies, geochemistry, mineralogy and deposition sequences." Journal of African Earth Sciences 150 (February 2019): 757–66. http://dx.doi.org/10.1016/j.jafrearsci.2018.10.004.

Full text

APA, Harvard, Vancouver, ISO, and other styles

21

Slim-Shimi, N., Y. Moëlo, S. Tlig, and C. Lévy. "Sulfide geochemistry and genesis of Chouichia and Ain el Bey copper deposits in northwestern Tunisia." Mineralium Deposita 31, no. 3 (March 1996): 188–200. http://dx.doi.org/10.1007/bf00204026.

Full text

APA, Harvard, Vancouver, ISO, and other styles

22

Slim-Shimi, N., Y. Mo�lo, S. Tlig, and C. L�vy. "Sulfide geochemistry and genesis of Chouichia and Ain el Bey copper deposits in northwestern Tunisia." Mineralium Deposita 31, no. 3 (March 1, 1996): 188–200. http://dx.doi.org/10.1007/s001260050023.

Full text

APA, Harvard, Vancouver, ISO, and other styles

23

Dhaoui, Z., N. Chkir, K. Zouari, F. Hadj Ammar, and A. Agoune. "Investigation of uranium geochemistry along groundwater flow path in the Continental Intercalaire aquifer (Southern Tunisia)." Journal of Environmental Radioactivity 157 (June 2016): 67–76. http://dx.doi.org/10.1016/j.jenvrad.2016.03.005.

Full text

APA, Harvard, Vancouver, ISO, and other styles

24

Ellouz, F., M. Masmoudi, J. P. Quisefit, and K. Medhioub. "Characteristics of trace elements in aerosols collected in Northern Tunisia." Physics and Chemistry of the Earth, Parts A/B/C 55-57 (January 2013): 35–42. http://dx.doi.org/10.1016/j.pce.2010.12.003.

Full text

APA, Harvard, Vancouver, ISO, and other styles

25

Arfaoui, A., and M. Montacer. "Organic geochemical study of Ypresian sediments at Jebel Ousselat, Tunisia." Geochemistry International 46, no. 10 (October 2008): 1023–37. http://dx.doi.org/10.1134/s0016702908100078.

Full text

APA, Harvard, Vancouver, ISO, and other styles

26

Farhat, Boutheina, Abdallah Ben Mammou, Lamia Kouzana, Ismail Chenini, Francesca Podda, and Giovanni De Giudici. "Groundwater Chemistry of the Mornag Aquifer System in NE Tunisia." Resource Geology 60, no. 4 (November 23, 2010): 377–88. http://dx.doi.org/10.1111/j.1751-3928.2010.00142.x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

27

Buccione, Roberto, Rabah Kechiched, Giovanni Mongelli, and Rosa Sinisi. "REEs in the North Africa P-Bearing Deposits, Paleoenvironments, and Economic Perspectives: A Review." Minerals 11, no. 2 (February 19, 2021): 214. http://dx.doi.org/10.3390/min11020214.

Full text

Abstract:

A review of the compositional features of Tunisia, Algeria, and Morocco phosphorites is proposed in order to assess and compare the paleoenvironmental conditions that promoted the deposit formation as well as provide information about their economic perspective in light of growing worldwide demand. Since these deposits share a very similar chemical and mineralogical composition, the attention was focused on the geochemistry of rare earth elements (REEs) and mostly on ΣREEs, Ce and Eu anomalies, and (La/Yb) and (La/Gd) normalized ratios. The REEs distributions reveal several differences between deposits from different locations, suggesting mostly that the Tunisian and Algerian phosphorites probably were part of the same depositional system. There, sub-reducing to sub-oxic conditions and a major REEs adsorption by early diagenesis were recorded. Conversely, in the Moroccan basins, sub-oxic to oxic environments and a minor diagenetic alteration occurred, which was likely due to a different seawater supply. Moreover, the drastic environmental changes associated to the Paleocene–Eocene Thermal Maximum event probably influenced the composition of Northern African phosphorites that accumulated the highest REEs amounts during that span of time. Based on the REEs concentrations, and considering the outlook coefficient of REE composition (Koutl) and the percentage of critical elements in ΣREEs (REEdef), the studied deposits can be considered as promising to highly promising REE ores and could represent a profitable alternative source for critical REEs.

APA, Harvard, Vancouver, ISO, and other styles

28

Bouraoui, F., S. Benabdallah, A. Jrad, and G. Bidoglio. "Application of the SWAT model on the Medjerda river basin (Tunisia)." Physics and Chemistry of the Earth, Parts A/B/C 30, no. 8-10 (January 2005): 497–507. http://dx.doi.org/10.1016/j.pce.2005.07.004.

Full text

APA, Harvard, Vancouver, ISO, and other styles

29

Tribovillard, Nicolas, Christian Dupuis, and Eric Robin. "Sedimentological and diagenetical conditions of the impact level of the Cretaceous/Tertiary boundary in Tunisia; no anoxia required." Bulletin de la Société Géologique de France 171, no. 6 (November 1, 2000): 629–36. http://dx.doi.org/10.2113/171.6.629.

Full text

Abstract:

Abstract The Ain Settara section (Kalaat-Senan area, Tunisia) shows a well-exposed and expanded Cretaceous/Tertiary (K/T) boundary that can be divided into several units of contrasted lithologies. The bolide impact level is identified thanks to the occurrence of a peak of iridium and Ni-rich spinel abundance. The impact level is a jarosite nodule-rich horizon upon which the emphasis is placed: the jarosite nodules, initially present as pyrite nodules, may be interpreted as reflecting reducing depositional conditions at the K/T boundary. Trace metal geochemistry indicates that depositional conditions were not reducing and that the nodules must not have formed during earliest diagenesis. Consequently, water column-scaled anoxia cannot be put forward to account for the mass extinctions observed at the K/T boundary at Ain Settara.

APA, Harvard, Vancouver, ISO, and other styles

30

Souissi, Fouad, Radhia Sassi, Jean-Louis Dandurand, Salah Bouhlel, and Sami Ben Hamda. "Fluid inclusion microthermometry and rare earth element distribution in the celestites of the Jebel Doghra ore deposit (Dome Zone, northern Tunisia): towards a new genetic model." Bulletin de la Société Géologique de France 178, no. 6 (November 1, 2007): 459–71. http://dx.doi.org/10.2113/gssgfbull.178.6.459.

Full text

Abstract:

Abstract The celestite ore of Jebel Doghra occurs as stratabound deposits within the cap-rock of a diapiric structure of Triassic salt-rocks. The celestite deposits result mainly from the late diagenetic to epigenetic replacement of the carbonated host-rocks giving rise to a dolomite-celestite “banded ore”. Celestite is locally observed within fractures. This study proposes a new genetic model based on fluid inclusion (FI) microthermometry and REE geochemistry. FI show that celestite, occurring either as stratabound bodies or lodes, was deposited from a highly saline (20.7 ± 1.3 wt%NaCl equivalents) and warm (174 ± 3oC) basinal fluid, which contains hydrocarbon droplets and CO2. The geochemistry of the REE shows that the deposition of celestite is due to the mixing between a deep-sourced fluid which has acquired high Sr concentrations by leaching feldspar-rich series in depth and a sulfate-rich solution associated with the Triassic evaporites.

APA, Harvard, Vancouver, ISO, and other styles

31

AKROUT, Dhaou, Hassène AFFOURI, Riadh AHMADI, Eric MERCIER, and Mabrouk MONTACER. "Source Rock Characterization and Petroleum Systems in North Ghadames Basin, Southern Tunisia." Resource Geology 61, no. 3 (June 23, 2011): 270–80. http://dx.doi.org/10.1111/j.1751-3928.2011.00163.x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

32

Smykatz-Kloss, W., H. Kossl, and H. Hotzl. "The gypsum karst area of Foum Tatahouine, Southern Tunisia: Mineralogy and hydrogeochemistry." Chemical Geology 84, no. 1-4 (July 1990): 206–7. http://dx.doi.org/10.1016/0009-2541(90)90214-r.

Full text

APA, Harvard, Vancouver, ISO, and other styles

33

Garnit, Hechmi, Salah Bouhlel, Donatella Barca, Craig A. Johnson, and Chaker Chtara. "Phosphorite-hosted zinc and lead mineralization in the Sekarna deposit (Central Tunisia)." Mineralium Deposita 47, no. 5 (December 17, 2011): 545–62. http://dx.doi.org/10.1007/s00126-011-0395-y.

Full text

APA, Harvard, Vancouver, ISO, and other styles

34

Abid, Kamel, Friha Hadj Ammar, Stephan Weise, Kamel Zouari, Najiba Chkir, Kazimierz Rozanski, and Karsten Osenbrück. "Geochemistry and residence time estimation of groundwater from Miocene–Pliocene and Upper Cretaceous aquifers of Southern Tunisia." Quaternary International 338 (August 2014): 59–70. http://dx.doi.org/10.1016/j.quaint.2014.04.036.

Full text

APA, Harvard, Vancouver, ISO, and other styles

35

Prudêncio, M. I., M. I. Gonzalez, M. I. Dias, E. Galan, and F. Ruiz. "Geochemistry of sediments from El Melah lagoon (NE Tunisia): A contribution for the evaluation of anthropogenic inputs." Journal of Arid Environments 69, no. 2 (April 2007): 285–98. http://dx.doi.org/10.1016/j.jaridenv.2006.10.006.

Full text

APA, Harvard, Vancouver, ISO, and other styles

36

Chakroun, A., J. C. Miskovsky, and D. Zaghbib-Turki. "Quartz grain surface features in environmental determination of aeolian Quaternary deposits in northeastern Tunisia." Mineralogical Magazine 73, no. 4 (August 1, 2009): 607–14. http://dx.doi.org/10.1180/minmag.2009.073.4.607.

Full text

APA, Harvard, Vancouver, ISO, and other styles

37

Fromm, Roman, Tarek Hachicha, and Werner Smykatz-Kloss. "Aridic crusts and vein mineralisations in the playa Areg el Makrzene, South Tunisia." Geochemistry 65, no. 4 (October 2005): 357–73. http://dx.doi.org/10.1016/j.chemer.2005.01.005.

Full text

APA, Harvard, Vancouver, ISO, and other styles

38

Hamdi Nasr, Imen, Adnen Amiri, Mohamed Hédi Inoubli, Abdelhmid Ben Salem, AbdelHak Chaqui, and Said Tlig. "Structural Setting of Northern Tunisia Insights from Gravity Data Analysis Jendouba Case Study." Pure and Applied Geophysics 168, no. 10 (August 31, 2010): 1835–49. http://dx.doi.org/10.1007/s00024-010-0189-7.

Full text

APA, Harvard, Vancouver, ISO, and other styles

39

Bahrouni, N., S. Bouaziz, A. Soumaya, N. Ben Ayed, K. Attafi, Y. Houla, A. El Ghali, and N. Rebai. "Neotectonic and seismotectonic investigation of seismically active regions in Tunisia: a multidisciplinary approach." Journal of Seismology 18, no. 2 (September 18, 2013): 235–56. http://dx.doi.org/10.1007/s10950-013-9395-y.

Full text

APA, Harvard, Vancouver, ISO, and other styles

40

Eloussaief, Mabrouk, Ikram Jarraya, and Mourad Benzina. "Adsorption of copper ions on two clays from Tunisia: pH and temperature effects." Applied Clay Science 46, no. 4 (December 2009): 409–13. http://dx.doi.org/10.1016/j.clay.2009.10.008.

Full text

APA, Harvard, Vancouver, ISO, and other styles

41

Ayadi, Yosra, Belgacem Redhaounia, Naziha Mokadem, Karim Zighmi, Mohamed Dhaoui, and Younes Hamed. "Hydro-geophysical and geochemical studies of the aquifer systems in El Kef region (Northwestern Tunisia)." Carbonates and Evaporites 34, no. 4 (June 30, 2018): 1391–413. http://dx.doi.org/10.1007/s13146-018-0460-z.

Full text

APA, Harvard, Vancouver, ISO, and other styles

42

Chairi, Raja, and Zohra El Asmi Djellouli. "Characterization of organic matter deposited in the oriental zone from Moknine hypersaline environment, oriental Tunisia." Chinese Journal of Geochemistry 24, no. 4 (October 2005): 345–51. http://dx.doi.org/10.1007/bf02873797.

Full text

APA, Harvard, Vancouver, ISO, and other styles

43

Ounis, Anouar, László Kocsis, Fredj Chaabani, and Hans-Rudolf Pfeifer. "Rare earth elements and stable isotope geochemistry (δ13C and δ18O) of phosphorite deposits in the Gafsa Basin, Tunisia." Palaeogeography, Palaeoclimatology, Palaeoecology 268, no. 1-2 (October 2008): 1–18. http://dx.doi.org/10.1016/j.palaeo.2008.07.005.

Full text

APA, Harvard, Vancouver, ISO, and other styles

44

Henchiri, Mohsen, and Nabil Fattah. "Extent of diagenetic transformations in severely altered biogenic silica deposits from Tunisia: new insights from mineralogy and geochemistry." Arabian Journal of Geosciences 7, no. 3 (January 9, 2013): 1179–86. http://dx.doi.org/10.1007/s12517-012-0827-8.

Full text

APA, Harvard, Vancouver, ISO, and other styles

45

Al-Aasm, Ihsan S., and Hassen Abdallah. "The origin of dolomite associated with salt diapirs in central Tunisia: Preliminary investigations of field relationships and geochemistry." Journal of Geochemical Exploration 89, no. 1-3 (April 2006): 5–9. http://dx.doi.org/10.1016/j.gexplo.2005.11.069.

Full text

APA, Harvard, Vancouver, ISO, and other styles

46

Baklouti, S., L. Maritan, Ll Casas, N. Laridhi Ouazaa, R. Jàrrega, M. Prevosti, C. Mazzoli, B. Fouzaï, S. Larabi Kassaa, and M. Fantar. "Establishing a new reference group of Keay 25.2 amphorae from Sidi Zahruni (Nabeul, Tunisia)." Applied Clay Science 132-133 (November 2016): 140–54. http://dx.doi.org/10.1016/j.clay.2016.05.027.

Full text

APA, Harvard, Vancouver, ISO, and other styles

47

Steinberg, Michel, Michel Rautureau, and Marc Rivière. "Analysis of zinciferous clays from central Tunisia using a scanning transmission electron microscope (STEM)." Chemical Geology 48, no. 1-4 (March 1985): 157–64. http://dx.doi.org/10.1016/0009-2541(85)90043-9.

Full text

APA, Harvard, Vancouver, ISO, and other styles

48

Montacer, M., J. R. Disnar, J. J. Orgeval, and J. Trichet. "Relationship between ZnPb ore and oil accumulation processes: Example of the Bou Grine deposit (Tunisia)." Organic Geochemistry 13, no. 1-3 (January 1988): 423–31. http://dx.doi.org/10.1016/0146-6380(88)90064-2.

Full text

APA, Harvard, Vancouver, ISO, and other styles

49

Ben Moussa, Amor, Sarra Bel Haj Salem, Kamel Zouari, and Fayçal Jlassi. "Hydrochemical and isotopic investigation of the groundwater composition of an alluvial aquifer, Cap Bon Peninsula, Tunisia." Carbonates and Evaporites 25, no. 3 (June 17, 2010): 161–76. http://dx.doi.org/10.1007/s13146-010-0020-7.

Full text

APA, Harvard, Vancouver, ISO, and other styles

50

Felhi, Mongi, Ali Tlili, and Mabrouk Montacer. "Geochemistry, Petrography and Spectroscopy of Organic Matter of Clay-Associated Kerogen of Ypresian Series: Gafsa-Metlaoui Phosphatic Basin, Tunisia." Resource Geology 58, no. 4 (December 2008): 428–36. http://dx.doi.org/10.1111/j.1751-3928.2008.00075.x.

Full text

APA, Harvard, Vancouver, ISO, and other styles

We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!