Skip to main content
Log in

Apatite-rich pyrometamorphic rocks from Suweileh area, Jordan

  • Original Paper
  • Published:
Arabian Journal of Geosciences Aims and scope Submit manuscript

Abstract

Representative samples from the upper Cretaceous pyrometamorphic rocks from Suweileh area were investigated by using XRD, XRF, SEM/EDS, and microprobe techniques. Suweileh area is characterized by the presence of varicolored marble (dominated by green apatite-rich rocks) overlying bituminous marl and silicified limestone-phosphorite beds. The bituminous rocks are enriched with P, S, and F in addition to reduced sensitive trace elements that were inherited later by their metamorphic equivalents. The rocks were affected by severe tectonism that produced intensive fracturing which facilitated the chemical leaching. The mineralogy of the varicolored marble from Suweileh area is equivalent to Daba-Siwaqa and Maqarin areas in central and north Jordan. High-temperature and low-temperature groups of minerals were recognized. The first group is the result of pyrometamorphism produced from the spontaneous combustion of bituminous marl. The metamorphism was contemporaneous with tectonism of the Rift Valley. The second secondary group of minerals is the result of alteration by high alkaline waters followed by precipitation along the weakness zones. A hyperalkaline circulating water similar to the current issuing waters from Maqarin (north Jordan) was responsible for leaching and precipitation of anions and trace elements. A similar scenario was reported in north and central Jordan. The calculated structural formula of fluorapatite is Ca5.02 (P2.325, Si0.22, S0.0833) O12 F0.975. The apatite structure incorporates S and Si (inherited from the bituminous precursor) that substitute for P in the tetrahedral positions.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14
Fig. 15

Similar content being viewed by others

References

  • Ajarmeh N (2014) Unusual mineralogy of Suweileh metamorphic rocks, Jordan. Unpublished M. Sc. thesis, The University of Jordan, Amman

  • Bender F (1968) Geologie Von Jordanian- BeitrageZurRegionalen Geologic Der Erde, vol 7. GebruderBorntraeger, Berlin, p 230

    Google Scholar 

  • Bender F (1974) Geology of Jordan. Borntraeger, Berlin, p 190

    Google Scholar 

  • Clark I, Firtz P, Seidlitz H, Khoury H, Trimborn P, Milodowski T, Pearce J (1993) Recarbonation of metamorphosed marls, Jordan. Appl Geochem 8:473–481

    Article  Google Scholar 

  • Clark I, Khoury H, Salameh E, Fritz P, Goksu Y, Wieser A, Causse C, Fontes J (1992) Travertines in central Jordan. IAEA—SM—319/6, 551–565

  • Elie M, Techer I, Trotignon L, Khoury H, Salameh E, Vandamme D, Boulvais P, Fourcade S (2007) Cementationof kerogen-rich marls by alkaline fluids released during weathering of thermally metamorphosed marly sediments. Part II: organic matter evolution, magnetic susceptibility and metals (Ti, Cr, Fe) at the Khushaym Matruck natural analogue (central Jordan). Appl Geochem 22:1311–1328

    Article  Google Scholar 

  • Fleurance S, Cuney M, Malartre M, Reyx J (2013) Origin of the extreme polymetallic enrichment (Cd, Cr, Mo, Ni, U, V, Zn) of the Late Cretaceous–Early Tertiary Belqa Group, central Jordan. Palaeogeogr Palaeoclimatol Palaeoecol 369:201–219

    Article  Google Scholar 

  • Khoury H (2002) Clays and clay minerals in Jordan. Publications of The University of Jordan. 116pp

  • Khoury H (2006) Industrial rocks and minerals in Jordan, Second edn. Publications of the University of Jordan. 346pp

  • Khoury H (2012) Long term analogue of carbonation in travertine from Uleimatquarries, central Jordan. Environ Earth Sci 65:1909–1916

    Article  Google Scholar 

  • Khoury H (2014) Importance of clay minerals in Jordan - case study: Volkonskoite as a sink for hazardous elements of a high pH plume. The Jordan Journal of Earth and Environmental Sciences (JJEES) 6(Special Publication 3):1–10

    Google Scholar 

  • Khoury H (2015) Uranium minerals of central Jordan. Applied Earth Science (Trans. Inst. Min. Metall. B). 124(2):104–128

    Article  Google Scholar 

  • Khoury, H, Abu Jayyab A (1995) Research note to the mineral volkonskoite: four new localities in central Jordan. Dirasat, The University of Jordan, 22B(1),189–198

  • Khoury H, Al-Zoubi A (2014) Origin and characteristics of Cr-smectite from Suweileh area, Jordan. Appl Clay Sci 90(2014):43–52

    Article  Google Scholar 

  • Khoury H, Eberl D (1979) Bubble-wall shards altered to montmorillonite. Clay Clay Miner 27(4):291–292. https://doi.org/10.1346/CCMN.1979.0270408

    Article  Google Scholar 

  • Khoury H, Mackenzie R, Russel J, Tait J (1984) An iron free volkonskoite. Clay Miner 19:43–57

    Article  Google Scholar 

  • Khoury H and Nassir S (1982a) A discussion on the origin of Daba-Siwaqamarble. Dirasat, vol 9. University of Jordan, pp 55–56

  • Khoury H, Nassir S (1982b) High mineralization in the bituminous limestone inMaqarin area, north Jordan. N Jb Miner Abh 144:187–213

    Google Scholar 

  • Khoury H, Salameh E (1986). The origin of high temperature minerals from Suweileh area. Dirasat, vol 13. University of Jordan, pp 261–269

  • Khoury H, Salameh E, Abdul-Jaber Q (1985) Characteristics of an unusual highly alkaline water from the Maqarin area, northern Jordan. J Hydrol 81:79–91

    Article  Google Scholar 

  • Khoury H, Salameh E, Clark I (2014) Mineralogy and origin of surficial uranium deposits hosted in travertine and calcrete from central Jordan. Appl Geochem 43:49–65

    Article  Google Scholar 

  • Khoury H, Salameh E, Clark F, Fritz R, Bajjali W, Miolodwski A, Cave M, Alexander W (1992) A natural analogue of high pH waters from the Maqarinarea of northern Jordan. 1: introduction to the site. J Geochem Explor 46:117–132

    Article  Google Scholar 

  • Khoury H, Sokol E, Clark I (2015) Calcium uranium oxides from Central Jordan: mineral assemblages, chemistry, and alteration products. Can Mineral 53(1):61–82

    Article  Google Scholar 

  • Khoury H, Sokol E, Kokh S, Seryotkin Y, Kozmenko O, Goryainov S, Clark I (2016a) Intermediate members of the lime-Monteponite solid solutions (Ca1-xCdxO, x = 0.36-0.55): discovery in natural occurrence. Am Mineral 101:146–161

    Article  Google Scholar 

  • Khoury H, Sokol E, Kokh S, Seryotkin Y, Nigmatulina E, Goryainov S, Belogub E, Clark I (2016b) Tululite, Ca14 (Fe3+, Al) (Al, Zn, Fe3+, Si, P, Mn, Mg)15O36: a new Ca zincate-aluminate from combustion metamorphic marbles, central Jordan. Mineral Petrol 110:125–140. https://doi.org/10.1007/s00710-015-0413-3

    Article  Google Scholar 

  • McDonald Sir M, Partners (1965) East Bank Water Resources, vol 6. Central water authority, Amman

    Google Scholar 

  • Mikbel S, Zacher W (1981) The Wadi Shueib structure in Jordan. N Jb Geol Palaont Abh 9:571–576

    Google Scholar 

  • Nassir S, Khoury H (1982) Mineralogy, petrology, and origin of Daba-Siwaqa marble, Jordan. Dirasat 9:107–130

    Google Scholar 

  • Powell J (1989) Stratigraphy and sedimentation of the Phanerozoic rocks in central and southern Jordan. Part B: Kurnub , Ajlun and Belqa groups. Bulletin 11B, Natural Resources Authority, Amman. 130

  • Powell J, Moh’d B (2011) Evolution of Cretaceous to Eocene alluvial and carbonate platform sequences in central and south Jordan. GeoArabia 16:29–82

    Google Scholar 

  • Sawariah A, Barjous M (1993) Geological map of Suweilih area, scale 1: 250,000, sheet no. 3154-II. Natural Resources Authority, Amman

    Google Scholar 

  • Sokol E, Kokh S, Khoury H, Seryotkin Y, Goryainov S (2016) Long-term immobilization of Cd2+ at the Tulul Al Hammam natural analogue site, central Jordan. Appl Geochem 70:43–60. https://doi.org/10.1016/j.apgeochem.2016.05.002

    Article  Google Scholar 

  • Sokol E, Kozmenko O, Khoury H, Kokh S, Novikova S, Nefedov A, Sokol I, Zaikin P (2017) Calcareous sediments of the Muwaqqar chalk marl formation, Jordan: mineralogical and geochemical evidences for Zn and Cd enrichment. Gondwana Res 46:204–226. https://doi.org/10.1016/j.gr.2017.03.008

    Article  Google Scholar 

  • Wiesemann G, Rosch H (1969) Das Apatit-Vorkommen von Suweilih (Nord-Jordanien). Beih Geol Jb 81:177–214

    Google Scholar 

Download references

Acknowledgements

The second author thanks Alexander von Humboldt Foundation, Germany (AvH), for supporting the analytical work in the Federal Institute for Geosciences and Natural Resources, Hannover (BGR), the Natural History Meuseum in Berlin (NHB), and the University of Ottawa, Canada. Special thanks are given to Mr. Yousef Abu Salha and Mr. Waddah Mahmoud from the Department of Geology, The University of Jordan, for their assistance in the SEM analysis.

Funding

The financial help of the Deanship of Academic Research, the University of Jordan, is highly appreciated.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Hani Khoury.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Al-Ajarmeh, N., Khoury, H. Apatite-rich pyrometamorphic rocks from Suweileh area, Jordan. Arab J Geosci 11, 520 (2018). https://doi.org/10.1007/s12517-018-3874-y

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12517-018-3874-y

Keywords

Navigation