Fluid circulation related to post-Miocene extension Thassos Island, North Aegean.

P. Boulvais; J.P. Brun; D. Sokoutis

doi:10.1111/j.1468-8123.2007.00171.x

Fluid circulation related to post-Miocene extension Thassos Island, North Aegean.

P. Boulvais, J.P. Brun, D. Sokoutis

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

In the North Aegean Domain, Thassos Island contains a Plio-Pleistocene basin controlled by a large-scale flat-ramp extensional system with a potential décollement located at depth within a marble unit. Numerous mineralizations associated with normal faults of Plio-Pleistocene age are the sign of fluid circulation during extension. Two main generations of fluid flow are recognized, related to Plio-Pleistocene extension. A first circulation under high-temperature conditions (about 100-200°C) resulted in dolomitization of marbles near the base of the Plio-Pleistocene basin. The dolomites are characterized by low δ

Original language	English
Pages (from-to)	159-170
Journal	Geofluids
Volume	7
DOIs	https://doi.org/10.1111/j.1468-8123.2007.00171.x
Publication status	Published - 2007

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10.1111/j.1468-8123.2007.00171.x

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title = "Fluid circulation related to post-Miocene extension Thassos Island, North Aegean.",

abstract = "In the North Aegean Domain, Thassos Island contains a Plio-Pleistocene basin controlled by a large-scale flat-ramp extensional system with a potential d{\'e}collement located at depth within a marble unit. Numerous mineralizations associated with normal faults of Plio-Pleistocene age are the sign of fluid circulation during extension. Two main generations of fluid flow are recognized, related to Plio-Pleistocene extension. A first circulation under high-temperature conditions (about 100-200°C) resulted in dolomitization of marbles near the base of the Plio-Pleistocene basin. The dolomites are characterized by low δ",

author = "P. Boulvais and J.P. Brun and D. Sokoutis",

year = "2007",

doi = "10.1111/j.1468-8123.2007.00171.x",

language = "English",

volume = "7",

pages = "159--170",

journal = "Geofluids",

issn = "1468-8115",

publisher = "Hindawi",

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T1 - Fluid circulation related to post-Miocene extension Thassos Island, North Aegean.

AU - Boulvais, P.

AU - Brun, J.P.

AU - Sokoutis, D.

PY - 2007

Y1 - 2007

N2 - In the North Aegean Domain, Thassos Island contains a Plio-Pleistocene basin controlled by a large-scale flat-ramp extensional system with a potential décollement located at depth within a marble unit. Numerous mineralizations associated with normal faults of Plio-Pleistocene age are the sign of fluid circulation during extension. Two main generations of fluid flow are recognized, related to Plio-Pleistocene extension. A first circulation under high-temperature conditions (about 100-200°C) resulted in dolomitization of marbles near the base of the Plio-Pleistocene basin. The dolomites are characterized by low δ

AB - In the North Aegean Domain, Thassos Island contains a Plio-Pleistocene basin controlled by a large-scale flat-ramp extensional system with a potential décollement located at depth within a marble unit. Numerous mineralizations associated with normal faults of Plio-Pleistocene age are the sign of fluid circulation during extension. Two main generations of fluid flow are recognized, related to Plio-Pleistocene extension. A first circulation under high-temperature conditions (about 100-200°C) resulted in dolomitization of marbles near the base of the Plio-Pleistocene basin. The dolomites are characterized by low δ

U2 - 10.1111/j.1468-8123.2007.00171.x

DO - 10.1111/j.1468-8123.2007.00171.x

M3 - Article

VL - 7

SP - 159

EP - 170

JO - Geofluids

JF - Geofluids

SN - 1468-8115

ER -

Fluid circulation related to post-Miocene extension Thassos Island, North Aegean.

Abstract

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