Author: Joseph P. Kopera
Publisher:
ISBN:
Category : Folds (Geology)
Languages : en
Pages : 244
Book Description
Electron Microprobe Monazite Geochronology and Structural Analysis of the Ortega Formation, Northern Tusas Mountains, New Mexico
Electron Microprobe (Ultrachron) Geochronology of Monazite from the Homestake Iron Formation, Lead, the Black Hills, South Dakota, U.S.A.
Author: Lindsay E. Chasten
Publisher:
ISBN:
Category :
Languages : en
Pages : 194
Book Description
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.
Publisher:
ISBN:
Category :
Languages : en
Pages : 194
Book Description
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
Author: Reinhard A. Wobus
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 28
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 28
Book Description
Structure, Petrology, and Geochronology of Middle Proterozoic Rocks in the Tusas Mountains of Northern New Mexico
Author: Peter B. Davis
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 264
Book Description
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 264
Book Description
Mesoproterozoic Deposition, Regional Metamorphism and Deformation in North-central New Mexico
Author: Lily S. Pfeifer
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 71
Book Description
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.
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 71
Book Description
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
Author: Arthur Montgomery
Publisher:
ISBN:
Category : Borings
Languages : en
Pages : 426
Book Description
Publisher:
ISBN:
Category : Borings
Languages : en
Pages : 426
Book Description
Stratigraphy of the Morrison Formation in Part of Northwestern New Mexico
Author: Val L. Freeman
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 32
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 32
Book Description
Geology of the Taos Region
Author: New Mexico Geological Society. Field Conference
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 454
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 454
Book Description
Geology of Part of the Southern Sangre de Cristo Mountains, New Mexico
Author: John Preston Miller
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 124
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 124
Book Description
Microprobe monazite geochronology
Author: M.L. Williams
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages :
Book Description