Inclusive evidence

Hedenquist, J.W. and Henley, R.W. (1985) The importance of CO2 on freezing point mea.surements of fluid inclusions evidence from active geothermal systems and implications for epithermal ore deposition. Econ. Geol, 50, 1379-1406. 

Wilde, A.R., Mernagh, T.P., Bloom, M.S., FIoffmann, C. 1989. Fluid inclusion evidence on the origin of some Australian unconformity-related uranium deposits. 

Bodnar, R. J. (1995). Fluid inclusion evidence for magmatic source of metals in porphyry copper deposits. Miner. Assoc. Canada, Short Course Series 23, 139—152. 

Rich R. A. (1979) Fluid inclusion evidence for Silurian evaporites in southeastern Vermont. Geol. Soc. Am. Bull. 90, 1628-1643. 

Gregg, J. M., Shelton, K. L., and Bauer, R. M., 1992, Geochemical and fluid inclusion evidence for regional alteration of Upper Cambrian carbonates by basinal fluids in southern Missouri source rocks in the southern Midcontinent in 1990 symposium on source rocks in the southern Midcontinent, Norman, OK, p. 313-320. 

Lowenstein, T.K. Spencer, R.J. (1990) Syndepositional origin of potash evaporates petrographic and fluid inclusion evidence. American Journal of Science 290, 1-42. 

Calcite cement typically pre-dates quartz cementation, as indicated by the lack of quartz overgrowths within calcite-cemented zones (Table 1). As abundant fluid inclusion evidence (see review in Walderhaug, 1994) strongly indicates that quartz cementation typically becomes significant at temperatures of 70-80°C, this is strong confirmation that most calcite cementation was completed at temperatures below around 0 C. 

Diagenetic carbonate cement in reservoir sandstones of the Oseberg Formation (Brent Group) in the Oseberg field, Norwegian North Sea, occurs as disseminated siderite and ankerite, and as massively calcite-cemented intervals. Other diagenetic features include extensive feldspar dissolution and K-feldspar, quartz, kaolinite and dickite cements. Conditions of carbonate cementation are constrained on the basis of textural, geochemical and fluid inclusion evidence. 

Aulstead, K.L. Spencer, R.J. (1985) Diagenesis of the Keg River Formation, northwestern Alberta fluid inclusion evidence. Bull. Can. Petrol. Geol., 33, 167-183. 

Tobin, R.C. (1991) Diagenesis, thermal maturation and burial history of the upper Cambrian Bonneterre dolomite, southeastern Missouri an interpretation of thermal history from petrographic and fluid inclusion evidence. Org. Geochem., 17, 143-151. 

Wojcik, K.M., Goldstein, R.H. Walton, A.W. (1994) History of diagenetic fluids in a distant foreland area. Middle and Upper Pennsylvanian, Cherokee basin, Kansas, USA fluid inclusion evidence. Geochim. Cos-mochim. Acta, 58, 1175-1191. 

Frezzotti ML, de Vivo B, Clocchiatti R (1991) Melt-mineral-fluid interactions in ultramafic nodules from alkaline lavas of Mount Etna (Sicily, Italy) melt and fluid inclusion evidence. J Volcanol Geotherm Res 47 209-219... 

BENTONITES FROM ISHIRINI (LIBYA) AS NATURAL ANALOGUES OF LONG TERM THERMAL AND CHEMICAL EFFECTS ISOTOPIC AND FLUID INCLUSION EVIDENCE... 

Derome, D., Cathehneau, M., Lhomme, T, Crmey, M. (2003). Fluid inclusion evidence of the differential migration of H2 and O2 in the McArthur River unconformity-type uranium deposit (Saskatchewan, Canada). Possible role on post-ore modifications of the host rocks. Journal of Geochemical Exploration, 7B-79, 525-530. 

George, S.C., Lisk, M., Eadington, P.J. (2004) Fluid inclusion evidence for an early, marine-sourced oil charge prior to gas-condensate migration, Bayu-1, Timor Sea, Australia. Marine and Petroleum Geology, 21, 1107-1128. 

Schubert, E, Diamond, L.W., Toth, T.M. (2007) Fluid-inclusion evidence of petroleum migration through a buried metamorphic dome in the Pannonian Basin, Hungary. Chemical Geology, 244,351-381. 

Samples from Dartmoor are, however, notably enriched in Li, Sn and B in comparison with those from Cairngorm, as is indicated by Li/Sr, Sn/Zr, B/Si and B/Ga paired-element plots. It is suggested that this may be due to widespread pervasive high-temperature metamorphic and formational water-rock interaction, which probably occurred prior to vein-type mineralization (see also fluid inclusion evidence of Rankin and Alderton ). 

Often, forensic chemists produce scientific evidence that can be described as either inclusive or exclusive. Recall the red fiber example mentioned earlier in the chapter. In that example, successive classification based on analytical data demonstrated that the red fiber from a crime scene belonged to the same class as fibers from a suspect s red nylon jacket. This is an example of inclusive evidence The jacket is included in the population of items that could have been the source of the fiber in question. Had the fibers from the jacket been found to have a cross section different from that of the fiber found at the scene, they would have been exclusionary evidence The jacket could not have been the source. 

General unknown Inclusive evidence Precedent Trier of fact... 

Inclusive evidence Evidence that by itself includes a person or a possibility. 

Microthermometric technique is discussed in detail by Roedder in the section oii laboratory technique in a chapter "Fluid inclusion evidence on the genesis of ores in sedimentary and volcanic rocks" in a three volume set entitled "Ores in Sediments, Sedimentary and Volcanic Rocks" edited by K.H. Wolf, to be published by Elsevier Pub. Co. 

Roedder E (1976) Fluid-inclusion evidence on the genesis of ores in sedimentary and volcanic rocks. In Wolf KH (ed) Handbook of strata-bound and stratiform ore deposits, vol 2. Elsevier, New York, pp 67-110 Roedder E (1979) Fluid inclusions as samples of ore fluids. In Barnes HL (ed) Geochemistry of hydrothermal ore deposits. Wiley, New York, pp 684-737 Roedder E (1984) Fluid inclusions. Mineralogical Society of America, Washington DC. Rev Mineral 12 644 pp... 

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