Analiza inkluzji fluidalnych w minerałach w skałach osadowych Polski – przegląd ogólny i uwagi

Jarmołowicz-Szulc, Katarzyna

doi:10.5604/08676143.1200427

Cited by 2 publications

(4 citation statements)

References 8 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…It cannot be excluded, therefore, that some nonfluorescent (one phase) inclusions observed, e.g., in B 13, dolomite could contain methane similarly to those proved in Bu 9, although the lack of adequate microthermometric studies exactly there has not confirmed this suggestion yet. The presence of methane in inclusions in anhydrite is also possible (although not proved) if we refer to some observations of anhydrite in the Paproć-Cicha Góra area [35,36]. What is important is that, CH 4 occurs in inclusions in anhydrite in the B 9 and in the Mo1 anhydrite, with the nitrogen admixture (compare: [31]).…”

Section: Discussionmentioning

confidence: 94%

See 1 more Smart Citation

Application of Fluid Inclusions to Petroleum Basin Recognition—A Case Study from Poland

Jarmołowicz-Szulc

2021

Minerals

Self Cite

View full text Add to dashboard Cite

Fluid inclusions were studied in rocks from different wells from the Barnówko–Mostno–Buszewo (BMB), the largest oil field in Poland and from the Lubiatów field. Sampling was performed at depths between about 3120–3220 m and 3221–3256 m, respectively. Different minerals (dolomite, calcite, anhydrite, quartz) reveal the presence of aqueous (AQFI) and hydrocarbon (HCFI) inclusions, the differentiation of which was checked by UV fluorescence and microthermometry. Inclusions occur in different abundances and are of variable character. The microthermometric studies of fluid inclusions resulted in the determination of temperatures of eutectic melting, ice melting, and homogenization. Based on the results obtained, three types of inclusions have been found. Two-phase non-fluorescent inclusions (AQFI) contain brines of differentiated salinity (from about 6 to 10 and from about 17 to 22 wt% NaCl equivalent). Two-phase fluorescent inclusions (HCFI 1) contain light mature oil of paraffin character. The oil is characterized by API gravity of about 41–42 degrees. Small one-phase non-fluorescent inclusions (HCFI 2) that homogenize in deep freezing contain methane with admixtures. The abundance of inclusions varies, depending on the mineral or well. They have been discussed in the context of hydrocarbon migration and accumulation.

show abstract

Section: Discussionmentioning

confidence: 94%

“…Fluid inclusion studies have been conducted for some years in some geological structures of the Polish Lowlands. Those studies concentrated mostly on diagenetic relations, e.g., in the Paproć-Cicha Góra field, close to the BMB region [35][36][37], or in the Lubiatów field itself [30].…”

Section: Discussionmentioning

confidence: 99%

Application of Fluid Inclusions to Petroleum Basin Recognition—A Case Study from Poland

Jarmołowicz-Szulc

2021

Minerals

Self Cite

View full text Add to dashboard Cite

show abstract

“…The pres ent study shows realgar, orpiment, cin na bar and non-ore goyazite and gyp sum. The quartz-carbon ate-bi tu men paragenesis (Jarmo³owicz-Szulc and Jankowski, 2011;Jarmo³owicz-Szulc et al, 2012) is seem ingly re lated to the tec tonic mélange zones while the ore min er al iza tion is gen er ally con nected with fis sures and dis lo ca tions. This min eral iza tion has an epigenetic char ac ter.…”

Section: Discussionmentioning

confidence: 99%

“…Such re search has been recently un der taken and partly re ported , to gether with fluid in clu sion stud ies. Ap pli ca tion of fluid in clu sion (FI) stud ies in min er als in sed imen tary bas ins may pro vide much data needed for re con struction of con di tions in volv ing the pres ence of hy dro car bons, of the com po si tion of gas phases, of mi gra tion pro cesses, and so on (e.g., Jarmo³owicz-Szulc and Jankowski, 2011;Jarmo³owicz-Szulc et al, 2012;Jarmo³owicz-Szulc, 2016).…”

Section: Introductionmentioning

confidence: 99%

Genetic relationship of minerals to fluid circulation in the Polish Carpathians – the Bystre Slice case study

JARMOŁOWICZ-SZULC,

KLECZYŃSKI,

KOZŁOWSKI

et al. 2024

View full text Add to dashboard Cite

As so ci ate Ed i tor: Tomasz Bajda Field work con ducted in the area of the Bystre Slice of the Pol ish Carpathians has al lowed the rec og ni tion and map ping of min eral as sem blages with re spect to a mélange zone. Ore min er al iza tion in the Cre ta ceous and Paleogene zones of the Bystre Slice, an a lyzed geochemically, petro graphi cally and min er al og i cally, in cludes epigenetic min er als such as realgar, orpiment and cin na bar, here char ac ter ized and their parageneses de scribed. Fluid in clu sions are dis tin guished in newly discov ered realgar crys tals, and microthermometric re sults al low a min er al og i cal se quence in the study area to be pro posed. The new min eral goyazite, pre vi ously not de scribed in the Carpathians, oc curs as solid in clu sions in the realgar crys tals, co-oc cur ring with kaolinite. The min er al iza tion likely re lates to a mag matic anom aly pres ent in the NE part of Slovakia in the West ern Carpathians south of Dukla in Po land, and a pos si ble sub-sur face subvolcanic body that deep ens to wards the E, the in ferred top of which lies at a depth of ~1 km. The min er al iza tion may be con nected with dis lo ca tions in the rock units.

show abstract

Analiza inkluzji fluidalnych w minerałach w skałach osadowych Polski – przegląd ogólny i uwagi

Cited by 2 publications

References 8 publications

Application of Fluid Inclusions to Petroleum Basin Recognition—A Case Study from Poland

Application of Fluid Inclusions to Petroleum Basin Recognition—A Case Study from Poland

Genetic relationship of minerals to fluid circulation in the Polish Carpathians – the Bystre Slice case study

Contact Info

Product

Resources

About