Origin of tonalites from the Boil Mountain ophiolitic complex, west-central Maine

Conference · Mon Mar 01 00:00:00 EST 1993 · Geological Society of America, Abstracts with Programs; (United States)

OSTI ID:5722592

Chow, J S ^[1]

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1. Boston Univ., MA (United States). Geology Dept.

The Boil Mountain ophiolitic complex, west-central Maine, marks the suture between the Boundary Mountain and Gander terranes that became amalgamated in the late Cambrian during a pre-Taconic collisional event known as the Penobscottian orogeny. This even formed a composite terrane that is believed to have collided with the proto-North American margin during the Ordovician Taconic orogeny. The ophiolite is unusual in that there is no associated tectonized ultramafic section; there is a lack of a sheeted dike sequence; and an intrusive tonalite layer comprises a significant volume of the complex. Preliminary major and trace element geochemical analysis of the tonalites indicates that this unit is derived by partial melting of the associated mafic volcanics. This melting may have been induced by stopping water-rich hydrothermally altered basalts into subcrustal magma chambers. The association of arc-like volcanics and plutonics of the Boil Mountain ophiolite with the adjacent Hurricane melange suggests that the Boil Mountain may be a fragment of a forearc supra-subduction zone complex. Similar interpretations have been made recently for the Late Proterozoic Bou Azzer ophiolite in Morocco and the Coast Range ophiolite.

• OSTI ID: 5722592
• Report Number(s): CONF-9303211-; CODEN: GAAPBC
• Journal Information: Geological Society of America, Abstracts with Programs; (United States), Vol. 25:2; Conference: 28. annual Geological Society of America (GSA) Northeastern Section meeting, Burlington, VT (United States), 22-24 Mar 1993; ISSN 0016-7592
• Country of Publication: United States
• Language: English

Related Subjects

58 GEOSCIENCES
GEOLOGIC FORMATIONS
PETROCHEMISTRY
PETROGENESIS
GRANODIORITES
MAINE
CAMBRIAN PERIOD
GEOLOGIC DEPOSITS
GEOLOGIC HISTORY
HYDROTHERMAL ALTERATION
METAMORPHISM
OROGENESIS
PLATE TECTONICS
SUBDUCTION ZONES
DEVELOPED COUNTRIES
GEOLOGIC AGES
GEOLOGY
GRANITES
IGNEOUS ROCKS
NORTH AMERICA
PALEOZOIC ERA
PETROLOGY
PLUTONIC ROCKS
ROCKS
TECTONICS
USA
580000* - Geosciences