Fluid inclusions in sedimentary and diagenetic systems

Goldstein, Robert H.

doi:10.1016/s0024-4937(00)00044-x

Cited by 439 publications

(221 citation statements)

References 35 publications

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“…The fol low ing fea tures can be de scribed for the si der it ic sam ples from the Czêstochowa re gion in the min er als from the Parkoszowice 58BN bore hole, which oc cur in a rel a tive nar row depth in ter val: one-phase in clu sion as so ci a tions in sideroplesite, which point to trap ping at tem per a tures of 40-50°C (Goldstein, 2001); vari a tion of ice melt ing tem per a tures in the in ter val from -5.3 to -9.7°C. The T m re sults for the rhombohedric sideroplesite are be tween -5.3 and -6.6°C, while those for the sideroplesite in ooids are from -5.3 to -9.7°C, that cor responds to sa lin ity in ter vals of be tween 7.8 and 10.5 wt.% NaCl eq.…”

Section: Temperature Measurementsmentioning

confidence: 99%

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Temperature and isotopic relations in carbonate minerals in the Middle Jurassic sideritic rocks of central and southern Poland

Jarmołowicz-Szulc

Kozłowska

2016

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1 Pol ish Geo log i cal In sti tute -Na tional Geo log i cal In sti tute, Rakowiecka 4, 00-975 Warszawa, Po land Jarmo³owicz-Szulc, K., Koz³owska, A., 2016. Tem per a ture and iso to pic re la tions in car bon ate min er als in the Mid dle Ju rassic si der it ic rocks of cen tral and south ern Po land. Geo log i cal Quar terly, 60 (4): 881-892, doi: 10.7306/gq.1323The pres ent study as sesses the physico-chem i cal char ac ter of the flu ids re spon si ble for the gen e sis of car bon ate min er als in the Mid dle Ju ras sic si der it ic rocks at the north east ern mar gin of the Holy Cross Mts. and in the Czêstochowa re gion. These rocks oc cur at pres ent at depths be tween 30 and 600 m. Fluid in clu sion and iso to pic anal y ses have been per formed in the car bon ate min er als from si der it ic sand stones, clayey siderites and si der it ic coquinas. Sid er ite is the main car bon ate min eral of the si der it ic rocks. Cal cite and an ker ite are also pres ent. The sid er ite is rep re sented by two va ri et ies, Mg-rich sid er ite (sideroplesite, less com monly -pistomesite) and sid er ite. Two gen er a tions of sid er ite have been dis tin guished -an early and a late one. The early sid er ite was formed at tem per a tures of about 20°C in the zone of mi cro bi o log i cal methanogenesis from ma rine wa ters with some in flu ence of me te oric wa ters (d 18 O from -7.84 to -1.92‰ VSMOW). The late sid er ite crys tallized at tem per a tures of about 62-110°C from pore wa ters en riched in 18 O (d 18 O >0‰ VSMOW) as com pared with the iso topic com po si tion of the wa ters re spon si ble for the early sid er ite gen er a tion. The con ducted fluid in clu sion anal y ses point to for ma tion of the ce ments from com plex flu ids of brine and car bon di ox ide char ac ter, with den si ties slightly ex ceed ing 1 g/cm 3 and sa lini ties vary ing from 10.5 to 16.9 wt.% NaCl eq. and from 6.4 to 14.0 wt.% NaCl eq. in the Holy Cross Mts. and in the Czêstochowa re gion, re spec tively. The ho mog e ni za tion tem per a tures lie in the in ter vals of 62-110°C and 60-97°C, re spectively and rep re sent el e vated val ues com pared with data from the Pol ish Low lands. Apart from burial, other heat sources must have been im por tant for the lithogenesis of the Mid dle Ju ras sic de pos its.Key words: fluid in clu sions, iso topes, car bon ate min er als, si der it ic rocks, Mid dle Ju ras sic.

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Section: Temperature Measurementsmentioning

confidence: 99%

“…In diagenetic stud ies, ther mo met ric in ter pre ta tion has to take into ac count a num ber of fac tors (Goldstein, 2001). First, the char ac ter of fluid in clu sions (pri mary or sec ond ary) needs to be con sid ered.…”

Section: Introductionmentioning

confidence: 99%

Temperature and isotopic relations in carbonate minerals in the Middle Jurassic sideritic rocks of central and southern Poland

Jarmołowicz-Szulc

Kozłowska

2016

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“…On the ba sis of the dis tri bu tion of fluid in clu sions that oc cupy the cen tral parts of type I, II and IV crys tals, it seems to be more prob a ble that the core of the crys tals rep re sents its pri mary part. Densely packed FIA sug gest rapid crys tal growth in the sed i men tary ba sin in favour able con di tions (Roedder, 1984a, b;Goldstein and Reynolds, 1994;Goldstein, 2001). Such con di tions may also be re spon si ble for the formation of large crystals, if the number of nuclei of crystallisation was low.…”

Section: Discussionmentioning

confidence: 99%

“…This pro cess is ev i denced by, e.g., lack of primary FIA or the fact that their rem nants are very rarely lo cated in the cen tre of some ha lite crys tals, by the pres ence of var i ous types of sec ond ary FIA (Fig. 9D) high light ing traces of healed frac tures (e.g., Roedder, 1984a, b;Goldstein and Reynolds, 1994;Goldstein, 2001;van der Kerkhof and Hein, 2001;Kovalevych and Vovnyuk, 2010), and the pres ence of un healed fractures (Fig. 9B).…”

Section: Discussionmentioning

confidence: 99%

The influence of tectonics on petrological characteristics of anhydrite and anhydrite-halite intercalations in the Oldest Halite (Na1) (Zechstein, Upper Permian) of the Bądzów area (SW Poland)

Toboła

2014

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Tobo³a, T., 2014. The in flu ence of tec ton ics on pet ro log i cal char ac ter is tics of anhydrite and anhydrite-ha lite in ter ca la tions in the Old est Ha lite (Na1) (Zechstein, Up per Perm ian) of the B¹dzów area (SW Po land). Geo log i cal Quar terly, 58 (3): 531-542, doi: 10.7306/gq.1171The Old est Ha lite (Na1) (Zechstein, Up per Perm ian) played a sig nif i cant role in the de vel op ment of geo log i cal struc ture of the Fore-Sudetic Monocline (SW Po land) be cause of its dif fer ent rhe o log i cal prop er ties in com par i son to the ad ja cent rocks. In ter ca la tions of anhydrite and anhydrite-ha lite oc cur ring within the Na1 show a lot of fea tures of tec toni cally dis turbed rocks. Mac ro scopic pet ro log i cal ob ser va tions re vealed that anhydrite rocks rep re sent four rock types with dif fer ent struc tural and tex tural prop er ties. On the mi cro scopic scale, five types of crys tals have been dis tin guished in all mac ro scopic types. They vary in size, shape and dis tri bu tion of pri mary fluid in clu sion as sem blages. The anhydrite-ha lite rocks show two groups with slightly dif fer ent pet ro log i cal fea tures that are ap par ently re lated to their tec tonic de for ma tion and recrystallisation processes. The main re corded di rec tions of tec tonic move ments seem to be hor i zon tal or sub-hor i zon tal.

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“…Em ambiente sedimentares, fluidos aquosos predominam e participam ativamente dos processos diagenéticos atuantes em uma bacia sedimentar (Goldstein, 2001). A análise de inclusões fluidas em minerais autigênicos tem fornecido informações valiosas para o entendimento da dinâmica e evolução de processos pós-deposicionais e apresenta-se como método de destaque no estudo de sistemas petrolíferos, por fornecer informações diretas acerca dos fluidos diagenéticos (Goldstein & Reynolds, 1994;Munz, 2001 (Zalán et al, 1990a).…”

Section: Introdução _________________________________________unclassified

Paleotemperaturas e paleofluidos da Formação Irati na borda leste da Bacia do Paraná: implicações para a geração e migração de hidrocarbonetos

Oliveira¹

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Fluid inclusions in sedimentary and diagenetic systems

Cited by 439 publications

References 35 publications

Temperature and isotopic relations in carbonate minerals in the Middle Jurassic sideritic rocks of central and southern Poland

Temperature and isotopic relations in carbonate minerals in the Middle Jurassic sideritic rocks of central and southern Poland

The influence of tectonics on petrological characteristics of anhydrite and anhydrite-halite intercalations in the Oldest Halite (Na1) (Zechstein, Upper Permian) of the Bądzów area (SW Poland)

Paleotemperaturas e paleofluidos da Formação Irati na borda leste da Bacia do Paraná: implicações para a geração e migração de hidrocarbonetos

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