The geochemical evolution of the proterozoic continental crust in northwestern Jiangxi and western Zhejiang, China

1993 ◽  
Vol 12 (4) ◽  
pp. 308-316
Author(s):  
Zhang Bangtong ◽  
Ling Hongfei ◽  
Zhang Zuhuan ◽  
Liu Jishun ◽  
Ni Qisheng ◽  
...  
Keyword(s):  
Continental Crust ◽  
Geochemical Evolution ◽  
Proterozoic Continental Crust

scholarly journals Geochemical Evolution of Earth's Continental Crust

2018 ◽  
Author(s):  
C. Brenhin Keller
Keyword(s):  
Continental Crust ◽  
Quantitative Information ◽  
Earth’S Crust ◽  
Geochemical Evolution ◽  
Geologic Time ◽  
Open Questions ◽  
Equable Climate ◽  
Earth's Crust ◽  
Life On Earth ◽  
Underlying Processes

Earth’s unique continental crust represents the active interface between the deep earth and the surface earth system, and is crucial for the survival and diversification of life on Earth, both as a source for nutrients and a component in the silicate weathering feedback that stabilizes Earth’s equable climate on billion-year timescales. However, many open questions remain regarding the formation and secular temporal evolution of Earth’s crust – in part due to the extremely poorly-mixed nature of Earth’s continental crust such that compositional heterogeneity at any one point in geologic time typically dwarfs any systematic variation over time. New computational approaches enabled by the emergence of large, freely accessible geochemical datasets provide a way to see through this heterogeneity and extract quantitative information about underlying processes and variables that drive the evolution of Earth’s crust over geologic time.

The geochemical evolution of the continental crust

1995 ◽  
Vol 33 (2) ◽  
pp. 241 ◽  
Author(s):  
Stuart Ross Taylor ◽  
Scott M. McLennan
Keyword(s):  
Continental Crust ◽  
Geochemical Evolution

A Discussion on global tectonics in Proterozoic times - Introductory remarks

1976 ◽  
Vol 280 (1298) ◽  
pp. 399-403
Keyword(s):  
Continental Crust ◽  
Horizontal Displacement ◽  
Polar Wander ◽  
Igneous Activity ◽  
Order Of Magnitude ◽  
Global Tectonics ◽  
Horizontal Displacements ◽  
Proterozoic Continental Crust

Palaeomagnetic measurements show that horizontal displacements of the crust occurred throughout the Proterozoic at rates comparable to those recorded from the Mesozoic to the present day. However, examination of Proterozoic continental crust reveals some structures which cannot be matched precisely at the present time. Proterozoic stable blocks are smaller and more numerous than the plates of the present day. Those blocks were surrounded by belts in which deformation and igneous activity occurred during times when the blocks behaved as rigid masses. When the apparent polar wander paths of these stable blocks are compared, they are seen to follow rather similar tracks implying that a number of isolated blocks followed approximately the same course. Bearing in mind the uncertainties in establishing pole positions and in dating the rocks concerned, Precambrian apparent polar wander paths are still not precisely located. Despite these uncertainties it would appear that a genuine phenomenon has been revealed which can be described in these terms. During Proterozoic times rates of divergence between stable blocks within a continental mass were an order of magnitude smaller than the overall rate of horizontal displacement of that mass.

scholarly journals Relationship between magmatic, metamorphic and hydrothermal processes within the Baikal-Muya terrane (Eastern Siberia): constraints from a high-precision geochronological study of the Kedrovsky granitoid massif

2019 ◽  
Vol 489 (3) ◽  
pp. 292-297
Author(s):  
A. V. Chugaev ◽  
I. V. Chernyshev ◽  
E. Y. Rytsk ◽  
E. B. Salnikova ◽  
A. A. Nosova ◽  
...  
Keyword(s):  
Continental Crust ◽  
High Precision ◽  
Gold Mineralization ◽  
Early Stage ◽  
Eastern Siberia ◽  
Crust Formation ◽  
Metasedimentary Rocks ◽  
Geochronological Study ◽  
Granitoid Massif ◽  
Proterozoic Continental Crust

High-precision dating of granitoids is significant for identification the ages of the main stages of crust formation in various blocks of the continental crust. In this work, we dating the Kedrovskiy diorite-granodiorite massif localized within the South Muya block of the Baikal-Muya accretion terrane (BMT) (Eastern Siberia) among the Neoproterozoic gabbroids of the Kedrovskiy complex and metasedimentary rocks of the Kedrovskaya Formation. The results of U-Pb (ID TIMS) and 39Ar-40Ar geochronological studies of the Kedrovskiy massif are discussed. The formation of the massif (781 3 Ma) occurred at an early stage formation of the Proterozoic continental crust of BMT during accretion of Baikalids with the Siberian craton. A later thermal event (626 11 Ma) of the Ediacaran stage evolution BMT is reflected in the formation of of biotite-quartz-feldspar veins that cut through the granitoids of the Kedrovka massif. The obtained geochronological data show that the gold mineralization of the Kedrovskiy deposit (273 4 Ma) was not generated by the Kedrovskiy massif granitoids.

scholarly journals Petrogenesis of Ore-Hosting Diorite in the Zaorendao Gold Deposit at the Tongren-Xiahe-Hezuo Polymetallic District, West Qinling, China

Minerals ◽  
2019 ◽  
Vol 9 (2) ◽  
pp. 76 ◽  
Author(s):  
Zong-Yang Gou ◽  
Hao-Cheng Yu ◽  
Kun-Feng Qiu ◽  
Jian-Zhen Geng ◽  
Ming-Qian Wu ◽  
...  
Keyword(s):  
Gold Deposit ◽  
Continental Crust ◽  
Active Continental Margin ◽  
West Qinling ◽  
Isotopic Analyses ◽  
Wide Range ◽  
Mantle Component ◽  
Hf Isotopic Composition ◽  
T Values ◽  
Proterozoic Continental Crust

The newly discovered Zaorendao gold deposit is in the Tongren-Xiahe-Hezuo polymetallic district in the westernmost West Qinling orogenic belt. The estimated pre-mining resource is approximately 13.6 t of Au at an average grade of 3.02 g/t. Mineralization is predominantly controlled by NW-trending and EW-trending faults within diorite intrusions and surrounding sedimentary rocks. In the present study, in situ zircon U–Pb geochronology and Lu–Hf isotopic analyses of the ore-hosting diorite at Zaorendao were measured using LA-ICP-MS. The data suggest that the diorite was emplaced at ca. 246.5 ± 1.9 Ma. The large variation of zircon Hf isotopic composition (ɛHf(t) values ranging from −12.0 to −1.8) indicates a two-stage model age (TDM2) that ranges from 1.4 Ga to 2.0 Ga. Such Lu–Hf isotopic compositions indicate that the diorite was dominantly derived from a Paleo- to Meso-Proterozoic continental crust. The wide range of εHf(t) and the presence of inherited zircon can be interpreted to suggest the mixing of Paleo- to Meso-Proterozoic continental crust with a mantle component. Combining such characteristics with the geochemistry of coeval rocks that are associated with the diorite, we therefore proposed that the gold-hosting Triassic diorite in the Zaorendao gold deposit formed in an active continental margin that was associated with the northward subduction of the paleo-Tethyan ocean.

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