Works matching IS 14688115 AND DT 2013 AND VI 13 AND IP 3

Results: 10

Issue Information.
Published in:
Geofluids, 2013, v. 13, n. 3, p. i, doi. 10.1111/gfl.12054
Publication type:
Article
Characteristics of CO2-driven cold-water geyser, Crystal Geyser in Utah: experimental observation and mechanism analyses.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 283, doi. 10.1111/gfl.12018
By:
- Han, W. S.;
- Lu, M.;
- McPherson, B. J.;
- Keating, E. H.;
- Moore, J.;
- Park, E.;
- Watson, Z. T.;
- Jung, N.-H.
Publication type:
Article
Simulation of the impact of faults on CO2 injection into sandstone reservoirs.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 344, doi. 10.1111/gfl.12029
By:
- Pasala, S. M.;
- Forster, C. B.;
- Deo, M.;
- Evans, J. P.
Publication type:
Article
Experimental determination of CePO4 and YPO4 solubilities in H2O- NaF at 800° C and 1 GPa: implications for rare earth element transport in high-grade metamorphic fluids.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 372, doi. 10.1111/gfl.12031
By:
- Tropper, P.;
- Manning, C. E.;
- Harlov, D. E.
Publication type:
Article
Breakthrough of contaminant plumes in saturated volcanic rock: implications from the Yucca Mountain site.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 273, doi. 10.1111/gfl.12035
By:
- Kelkar, S.;
- Srinivasan, G.;
- Robinson, B. A.;
- Roback, R.;
- Viswanathan, H.;
- Rehfeldt, K.;
- Tucci, P.
Publication type:
Article
Hydrogeochemical dynamics affecting steam-heated pools at El Chichón Crater (Chiapas - Mexico).
Published in:
Geofluids, 2013, v. 13, n. 3, p. 331, doi. 10.1111/gfl.12028
By:
- Cuoco, E.;
- Francesco, S.;
- Tedesco, D.
Publication type:
Article
Deformation bands and their impact on fluid flow in sandstone reservoirs: the role of natural thickness variations.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 359, doi. 10.1111/gfl.12030
By:
- Rotevatn, A.;
- Sandve, T. H.;
- Keilegavlen, E.;
- Kolyukhin, D.;
- Fossen, H.
Publication type:
Article
Geodynamic processes in the NW Bohemian swarm earthquake region, Czech Republic, identified by continuous gas monitoring.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 305, doi. 10.1111/gfl.12027
By:
- Weinlich, F. H.;
- Stejskal, V.;
- Teschner, M.;
- Poggenburg, J.
Publication type:
Article
The sources and formation processes of brines from the Lunnan Ordovician paleokarst reservoir, Tarim Basin, northwest China.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 381, doi. 10.1111/gfl.12033
By:
- Chen, J.;
- Liu, D.;
- Peng, P.;
- Yu, C.;
- Zhang, B.;
- Xiao, Z.
Publication type:
Article
In situ decarboxylation of acetic and formic acids in aqueous inclusions as a possible way to produce excess CH4.
Published in:
Geofluids, 2013, v. 13, n. 3, p. 298, doi. 10.1111/gfl.12026
By:
- Ong, A.;
- Pironon, J.;
- Robert, P.;
- Dubessy, J.;
- Caumon, M.-C.;
- Randi, A.;
- Chailan, O.;
- Girard, J.-P.
Publication type:
Article

Works matching IS 14688115 AND DT 2013 AND VI 13 AND IP 3

Issue Information.

Characteristics of CO<sub>2</sub>-driven cold-water geyser, Crystal Geyser in Utah: experimental observation and mechanism analyses.

Simulation of the impact of faults on CO<sub>2</sub> injection into sandstone reservoirs.

Experimental determination of CePO<sub>4</sub> and YPO<sub>4</sub> solubilities in H<sub>2</sub>O- NaF at 800° C and 1 GPa: implications for rare earth element transport in high-grade metamorphic fluids.

Breakthrough of contaminant plumes in saturated volcanic rock: implications from the Yucca Mountain site.

Hydrogeochemical dynamics affecting steam-heated pools at El Chichón Crater (Chiapas - Mexico).

Deformation bands and their impact on fluid flow in sandstone reservoirs: the role of natural thickness variations.

Geodynamic processes in the NW Bohemian swarm earthquake region, Czech Republic, identified by continuous gas monitoring.

The sources and formation processes of brines from the Lunnan Ordovician paleokarst reservoir, Tarim Basin, northwest China.

In situ decarboxylation of acetic and formic acids in aqueous inclusions as a possible way to produce excess CH<sub>4</sub>.