Electron Microprobe Monazite Geochronology and Structural Analysis of the Ortega Formation, Northern Tusas Mountains, New Mexico

Electron Microprobe Monazite Geochronology and Structural Analysis of the Ortega Formation, Northern Tusas Mountains, New Mexico PDF Author: Joseph P. Kopera
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ISBN:
Category : Folds (Geology)
Languages : en
Pages : 244

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Electron Microprobe (Ultrachron) Geochronology of Monazite from the Homestake Iron Formation, Lead, the Black Hills, South Dakota, U.S.A.

Electron Microprobe (Ultrachron) Geochronology of Monazite from the Homestake Iron Formation, Lead, the Black Hills, South Dakota, U.S.A. PDF Author: Lindsay E. Chasten
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ISBN:
Category :
Languages : en
Pages : 194

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Monazite dating of rocks in the Black Hills area has led to a better understanding of the timing of tectonic events and episodes of mineral growth. However, detailed geochronologic studies have not been done on rocks from the Homestake Iron Formation. The objective of this study was to constrain the age of mineralization by analyzing monazite in rocks of the Homestake Formation, and to relate these ages to textures and episodes of mineral growth. Thin sections were investigated that represent a range of metamorphic conditions. Monazite was identified optically and using a scanning electron microscope, then U-Th-Pb dated with the Ultrachron. X-ray chemical maps were used to identify potential domains for which chemical ages were calculated. An allanite to monazite reaction was trapped in garnet that displayed yttrium zonation, indicating exhaustion of the allanite REE source during garnet growth. The reaction yields an age of 1757 ± 30 Ma, consistent with regional D2 related to the Trans-Hudson Orogen (THO). several regional tectonic events are represented by monazite ages in this study. A ~1850 Ma age of one monazite grain may be attributed to early southern THO activity, such as collission between the Wyoming craton and Dakota block. Regional D1 and D2 ages are well-represented. The ~1775 Ma ages are associated with D1 Yavapai island-arc collision to the south of the Black Hills. Some ~1670 Ma ages may have formed during far-field Mazatzal deformation to the south of the Yavapai terrane. The ~1715 Ma ages associated with intrusion of the Harney Peak Granite are prevalent in the Black Hills are considered a minimum age for mineralization. These ages have not yet been found in the Homestake Formation. This may be due to lower temperatures during mineralization that did not intersect a stability range of monazite, which experimentally forms at low temperatures and at a higher amphibolite facies grade. Several ~1300 and ~1200 Ma ages occur in lower-grade rocks and may have formed in the low-temperature stability range of monazite during the slow cooling period of the Black Hills.

Changes in the Nomenclature and Stratigraphy of Proterozoic Metamorphic Rocks, Tusas Mountains, North-central New Mexico

Changes in the Nomenclature and Stratigraphy of Proterozoic Metamorphic Rocks, Tusas Mountains, North-central New Mexico PDF Author: Reinhard A. Wobus
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 28

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Structure, Petrology, and Geochronology of Middle Proterozoic Rocks in the Tusas Mountains of Northern New Mexico

Structure, Petrology, and Geochronology of Middle Proterozoic Rocks in the Tusas Mountains of Northern New Mexico PDF Author: Peter B. Davis
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ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 264

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Mesoproterozoic Deposition, Regional Metamorphism and Deformation in North-central New Mexico

Mesoproterozoic Deposition, Regional Metamorphism and Deformation in North-central New Mexico PDF Author: Lily S. Pfeifer
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ISBN:
Category : Geology
Languages : en
Pages : 71

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Detrital zircon and metamorphic monazite ages from the Picuris Mountains, north central New Mexico, were used to confirm the depositional age of the Marquenas Formation, to document the depositional age of the Vadito Group, and to constrain the timing of metamorphism and deformation in the region.

Geology of the Thoreau Quadrangle, McKinley and Valencia Counties, New Mexico

Geology of the Thoreau Quadrangle, McKinley and Valencia Counties, New Mexico PDF Author: Arthur Montgomery
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Category : Borings
Languages : en
Pages : 426

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Stratigraphy of the Morrison Formation in Part of Northwestern New Mexico

Stratigraphy of the Morrison Formation in Part of Northwestern New Mexico PDF Author: Val L. Freeman
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Category : Geology
Languages : en
Pages : 32

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Geology of the Taos Region

Geology of the Taos Region PDF Author: New Mexico Geological Society. Field Conference
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Category : Geology
Languages : en
Pages : 454

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Geology of Part of the Southern Sangre de Cristo Mountains, New Mexico

Geology of Part of the Southern Sangre de Cristo Mountains, New Mexico PDF Author: John Preston Miller
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Category : Geology
Languages : en
Pages : 124

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Microprobe monazite geochronology

Microprobe monazite geochronology PDF Author: M.L. Williams
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Category :
Languages : en
Pages :

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