000 01999nam a2200241Ia 4500
003 MX-MdCICY
005 20250625160147.0
040 _cCICY
090 _aB-16243
245 1 0 _aMineral Deposits Associated with Stromatolites
490 0 _vDevelopments in Sedimentology. Chapter 11.1, 20(C), p.645-662, 1976
520 3 _aThis chapter discusses mineral deposits associated with stromatolites. The process of mineralization of stratiform deposits associated with stromatolites is an integral part of the development of sedimentary basins during sedimentation and diagenesis, and it is perhaps significant that many of the deposits discussed are in intracratonic basins. This chapter highlights where mineral deposits are formed, the contribution of the microorganisms can be indirect, helping to create a favorable physical and chemical environment, or more direct in trapping enriched material, helping to precipitate the valuable elements organically, or supplying other necessary elements such as sulphur. Alternatively, the organisms can merely survive in an environment where deposition of these elements is taking place, without playing any part in the process. After sedimentation and the diagenetic period, mineralization take place through the agency of connate brines that leach the valuable elements from their wide dispersion or from already-formed deposits, or through brines bringing them from a source external to the sediments; the brines would move, up-dip, till precipitation takes place in a favorable environment.
650 1 4 _aARIDITY EPISODE
650 1 4 _aFOSSIL STROMATOLITE
650 1 4 _aHOLOCENE (LATE)
650 1 4 _aHYDROLOGICAL HISTORY
650 1 4 _aISOTOPIC DATA
650 1 4 _aWATER BUDGET
700 1 2 _aMendelsohn, F.
856 4 0 _uhttps://drive.google.com/file/d/1Mh35gZgvnWu5JnjEJqZo8xBrLaovRnIb/view?usp=drivesdk
_zPara ver el documento ingresa a Google con tu cuenta: @cicy.edu.mx
942 _2Loc
_cREF1
008 250602s9999 xx |||||s2 |||| ||und|d
999 _c50417
_d50417