TIERCELIN, JJ and STOFFERS, P and MAKASU, MM and NDONTONI, Z and NZOJIBWAMI, E and BOULEGUE, J and CASTREC, M and PFLUMIO, C and SEIFFERT, G and NKIMBA, K and MINZANGI, K and ROLET, J and GENTE, P and COUSSEMENT, C and BUKU, S and MIFUNDU, W and BANDORA, T and MULLER, J and ZEILER, M and SABUKU, S and STETTER, KO and HUBER, R and ELSGAARD, L and MUKWAYA, G and GENTE, P and BIROLLEAU, A and HUGO, B and LECORFF, JJ and MUKWAYA, G and POUSSE, D and POUSSE, JF and SEIFFERT, G and TIERCELIN, JJ and VOLAT, JL (1992) SUBLACUSTRINE HYDROTHERMAL ACTIVITY AND MASSIVE SULFIDES FROM THE NORTH TANGANYIKA TROUGH, EAST-AFRICAN RIFT - 1991 TANGANYDRO EXPEDITION. COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II, 315 (6). pp. 733-740. ISSN 1251-8069,
Full text not available from this repository.Abstract
Intense sublacustrine hydrothermal activity has been investigated by scuba diving during the TANGANYDRO project along the Zaire side of the north Tanganyika trough (East African Rift). At the Pemba site, the vents are characterized by fluids with a temperature between 53 and 88-degrees-C, associated with iron sulfide veins. At Cape Banza site, the activity is characterized by aragonite chimneys and fluids with a temperature varying between 66 and 103-degrees-C. These hydrothermal vents are located at the intersection of N135 or N180 Precambrian cleavage, and N45 to N90 transverse fractures recently reactivated.
| Item Type: | Article |
|---|---|
| Uncontrolled Keywords: | DISCOVERY; |
| Depositing User: | Dr. Gernot Deinzer |
| Last Modified: | 19 Oct 2022 08:44 |
| URI: | https://pred.uni-regensburg.de/id/eprint/54386 |
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