4 edition of Vincent thrust, eastern San Gabriel Mountains, California found in the catalog.
Vincent thrust, eastern San Gabriel Mountains, California
James George Evans
|Statement||by James G. Evans.|
|Series||Geological Survey bulletin ;, 1507|
|LC Classifications||QE75 .B9 no. 1507, QE606.5.U6 .B9 no. 1507|
|The Physical Object|
|Pagination||15 p. :|
|Number of Pages||15|
|LC Control Number||81607914|
C.E JacobsonRelationship of deformation and metamorphism of the Pelona Schist to movement on the Vincent thrust, San Gabriel Mountains, southern California Am. J. Sci., (), pp. Google Scholar. Add to Book Bag Remove from Book Bag Saved in: Thrust-induced collapse of mountains an example from the "Big Bend" region of the San Andreas Fault, western Transverse Ranges, California /.
It is located along the trace of the Vincent Thrust in the San Gabriel Mountains of southern California. Mineralization occurs in the northeast-striking, 15? to 30? northwest-dipping Vincent Thrust zone. The thrust forms the contact between upper plate San Gabriel Gneiss (Precambrian) and lower plate Pelona Schist. (Precambrian or Mesozoic?). More than potassium-argon apparent ages on minerals from crystalline rocks, chiefly from the San Bernardino and eastern San Gabriel Mountains and the southern Mojave Desert, define an area greater t km 2 in which the potassium-argon isotopic systematics have been highly disturbed. The disturbance or disturbances appear to have culminated at different times in different parts of.
Desert, southern California: U.S. Geological Survey Professional Paper , 30 p. Nourse, J.A., , Middle Miocene reconstruction of the central and eastern San Gabriel Mountains, southern California, with implications for evolution of the San Gabriel Fault, and Los Angeles basin, in Barth, A., editor, Contributions to crustal. the Vincent Thrust, a major tectonic feature of the San Gabriel Mountains and eastern Transverse Ranges. This segment is about 2 miles north of the deposit. Few faults have been mapped otherwise in this immediate area. At the deposit proper, the plutonic .
Randy has diabetes
Teachers notes on Ọpuru áḍírí Ọgbia.
Spartanburg County marriages, 1785-1911
Songs of the heather heights.
practical treatise on casting and founding
A brief and true narration of the late wars risen in New-England
comparison of classroom climate in regular and French immersion primary classes
Integrated watershed management
Measurement in physical education
evaluation of the program of a typical womens club as a community project
The Vincent thrust is exposed for 24 km in the eastern San Gabriel Mountains, California (fig.1), between the Vincent Gap area on the west and North Fork Lytle Creek on the east; a small isolated sliver of the thrust also occurs in Middle Fork Lytle by: 2.
The Vincent thrust, eastern San Gabriel Mountains, California: A description of constituent metamorphic rock types of the upper and lower plates (Geological Survey bulletin) [James George Evans] on *FREE* shipping on qualifying offers.
Get this from a library. The Vincent thrust, eastern San Gabriel Mountains, California: a description of constituent metamorphic rock types of the upper and.
Get this from a library. The Vincent thrust, eastern San Gabriel Mountains, California. [James George Evans; Geological Survey (U.S.),]. The Vincent thrust, eastern California book Gabriel Mountains, California / by James G.
Evans. An edition of The Vincent thrust, eastern San Gabriel Mountains, California () The Vincent thrust, eastern San Gabriel Mountains, California a description of constituent metamorphic rock types of the upper and lower plates by James George EvansPages: The Vincent thrust, eastern San Gabriel Mountains, California by James George Evans, unknown edition.
General Information. Title: The Vincent thrust, eastern San Gabriel Mountains, California Author(s): Evans, J.G. Publishing Organization: U.S. Geological Survey Series and Number: Bulletin Publication Date: Map Scale:Cross Section: Yes North Latitude: 34° 23' 6" N () South Latitude: 34° 13' 19" N () East Longitude: ° 31' 26" W Vincent thrust.
Andrew P. Barth, "Chapter 3: Mid-crustal emplacement ofMesozoic plutons, San Gabriel Mountains, California, and implicationsfor the geologic history of the San Gabriel terrane", The Nature and Origin of Cordilleran Magmatism, J. Lawford Anderson. eastern San Gabriel Mountains that has been the subject of many studies in the last few decades.
Geologic mapping by Dibblee (), Morton (), Ehlig (, ), Nourse (unpublished mapping, ), Jacobson (), LaMascus (unpublished mapping, ), and Jones (unpublished mapping, ).
Geology and Mineral Wealth of the California Transverse Ranges Issue 10 of Annual field trip guidebook Issue 10 of Annual symposium and guidebook: Contributor: South Coast Geological Society: Publisher: South Coast Geological Society, Original from: the University of California: Digitized: Length: pages: Export Citation.
Buy The Vincent thrust, eastern San Gabriel Mountains, California: A description of constituent metamorphic rock types of the upper and lower plates (Geological Survey bulletin) by James George Evans (ISBN:) from Amazon's Book Store.
Everyday low prices and free delivery on eligible : James George Evans. The San Gabriel Mountains (Spanish: Sierra de San Gabriel) are a mountain range located in northern Los Angeles County and western San Bernardino County, California, United States. The mountain range is part of the Transverse Ranges and lies between the Los Angeles Basin and the Mojave Desert, with Interstate 5 to the west and Interstate 15 to the east.
The range lies in, and is surrounded. The Vincent thrust, eastern San Gabriel Mountains, California: a description of constituent metamorphic rock types of the upper and lower plates [James George Evans] on *FREE* shipping on qualifying : James George Evans.
the eastern San Gabriel Mountains (Premo et al., ; personal commun. with J. Nourse, in Hoyt et al., 20 18). The Proterozoic basement of southern California is intruded by numerous.
The evidence for such a claim stems from the relation between the present-day Banning and San Gabriel faults with an ancient thrust fault known as the Vincent Thrust.
This thrust fault appears both in the San Gabriel Mountains and the San Bernardino Mountains, near each of the supposed sections of the ancestral San Gabriel fault in such a way. The east-central San Gabriel Mountains reveal a folded stack of crystalline sheets constituting the lower and upper plates of the latest Cretaceous-Paleocene Vincent thrust (Figs.
2 and 3). shown in Figure 4. The San Gabriel Mountains, as outlined above, will be designated tectonically as the “San Gabriel uplift” (Dibblee, ). The San Gabriel Mountains uplift is highest in its eastern part, where it narrows and wedges out eastward into an alluvial plain.
This part includes its highest point, Mount San Antonio. The basement rocks of the eastern San Gabriel Mountains have been the subject of many studies in the last several decades. The Pelona Schist in this region is disrupted by both NE-striking and NW-striking fault systems that intersect one another.
The nature of intersections of such faults in the eastern San Gabriel Mountains is enigmatic. Does. The San Gabriel Mountains (SGM) is an east–west trending range formed from the uplift of the basement rocks along the southwest side of the ‘big bend’ portion of the SAF ().Recent fission track and U–Th/He analysis by Blythe et al.
() suggest that the high elevations (–3 km) of the SGM are largely uplifted within the last 7 Ma, with differential uplift patterns (including rate. The Rinconada and related faults in the southern coast ranges, California, and their tectonic significance / by: Dibblee, T. W.Published: () The Vincent thrust, eastern San Gabriel Mountains, California / by: Evans, James George, Published: ().
This age assignment suggests that the Mill Canyon mylonites are correlative with the Vincent thrust mylonites in the eastern San Gabriel Mountains (Jacobson et al., ). The gneissic, granitic, and sedimentary rocks of the San Gabriel Mountains lie within the upper plate of the Vincent thrust (e.g., Ehlig, ).
The lower plate is composed of Pelona Schist, which is predominantly meta-arkose (Haxel and Dillon, ; Ehlig, ; Jacobson et al., ).
This relationship is exposed in a structural window in the.