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Soft domination. Chinese Sim. Role playing. Behind me was Kowloon, a wall of dense grid-like apartment blocks with thumping basketball courts, chess players and trees filled with twittering sparrows.
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I resented the curt waiters Hong Kong service is often brusque at best , marvelled at the zen-like tai chi practitioners, and was surprised, at night, to stumble upon a gang of sex toy hawkers just off Nathan Road who laid their plastic goods out next to a row of fortune tellers. Several floors below the rooftop garden, railway passengers were setting off on cross-border trains bound for 44 mainland stations, including Shanghai , Kunming and Guilin. West Kowloon itself is impressive, but not without controversy.
Part of the station is under the control of Chinese police and customs officials , allowing for immigration checks before departure. But the immigration process was swift, friendly enough and easy. On board the Vibrant Express, smartly dressed stewards passed through the spotless carriage, offering tea in large glass cups with cork stoppers. The outside world was hushed and shut off, like a silenced TV set.
We eased into Guangzhou South. Passengers, faces melded to mobile phones, disembarked, one collective army of luggage-bearers, and headed up a broad staircase. Below, rows of platforms and identical snow white high-speed trains stretched as far as the eye could see. As the doors closed on the Vibrant Express, a team of men set to work, scrubbing the sides of the train by hand. The crowd tapered towards a colossal, bright-white concourse that resembled an insanely busy airport terminal.
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Even without the crowds, Guangzhou South would be disorientating. Eventually, my phone latched on and I found my pre-arranged guide, a well-travelled young Chinese woman who insisted I call her Jane, even though her Cantonese name translated beautifully as purple summer. Instead, the upwelling asthenosphere led to the partial melting of the subducted slab, which was then mixed with the ancient lower crust. The hybrid magma ascended to the upper crust, and intensive fractional crystallization or, potentially, upper-crustal assimilation resulted in low Ba:Th and La:Sm, weak NTT anomalies, and A-type granites; the eastern Hebei region was under an extensional tectonic setting with a thinning crust Fig 14B.
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The NIC is the pre-eminent example of the connection between hydrothermal-style gold mineralization and shoshonitic magma. It contains all the features that are considered to be optimal for the formation of economic, hydrothermal-style gold deposits, which contain shallowly emplaced high potassium calc-alkaline magmas with petrographic and chemical proof for abundant internal fractionation and depict differentiation that affords the build-up and retention of volatiles and metals in a fraction of the residual melt before volatile exsolution. A similar relation is observed in the northern margin of the NCC during the late Mesozoic with A-type granites containing large-scale polymetallic mineralization [ 84 — 87 ].
It is generally assumed that specific tectonic settings are associated with gold—copper—molybdenum mineralization; intra-plate setting related deposits depict similar mineral associations in northeastern NCC [ 1 , 88 — 90 ]. The generation of these deposits is assumed to be the result of crustal extension and lithospheric thinning during the Late Jurassic in NE China [ 19 , 32 , 36 — 38 , 62 , 91 , 92 ]. Many studies have indicated that crustal thickening and shortening with a compressional regime occurred in the NE China during Jurassic time [ 37 , 38 , 93 , 94 ].
They are suggested by large-scale contractional deformations and other thrusts along the Solonker—Xar Moron—Changchun—Yanji suture e. During Early Cretaceous time, the tectonic regime transformed from compressional to extensional as evidenced by large-scale emergence of the early Cretaceous metamorphic core complexes MCCs; e. The initial time of crustal thinning is usually considered to be at — Ma, interpreted to be related to the subduction of Paleo-Pacific Plate, with peak time at — Ma [ , ].
Moreover, early Cretaceous granites were widespread in northern part of the NCC, indicating extension predominantly occured in early Cretaceous S3 Table [ 23 , , ].
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These features provide robust proof that Late Jurassic was the transition time of the crustal from thickening to thinning. As stated previously, the occurrences of the mineralization and the zircon U—Pb ages of the A-type granites indicate that the mineralization was likely be formed by hydrothermal replacement during lithospheric thinning due to hybrid magma ascending to the upper crust, which caused the formation of the A-type granites [ 67 , 68 , 78 , 80 , 92 ]. Because of the spatial and temporal relations of the Au—Cu—Mo mineralization and the tectonic settings in which it occurs, we consider that the Au—Cu—Mo mineralization of Late Jurassic age along the northern margin of the NCC was likely to be related to lithospheric thinning after the continuing subduction of the paleo-Pacific plate [ — ].
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Recent mapping indicates that granites of the Mesozoic age are widespread throughout this region [ 21 , — ] S3 Table. Among the mineralization ages along the northern margin of the NCC, the establishment of a Late Jurassic age should stimulate renewed exploration to discover new Au—Cu—Mo resources. Thanks are due to Prof. Li Su for zircon U-Pb isotope and whole-rock trace-element analysis and staffs of Huajian gold deposit for their help in our field work.
The authors would also like to thank anonymous reviewers for their thorough, helpful, and constructive comments. The authors would like to thank Enago for the English language review. Browse Subject Areas? Click through the PLOS taxonomy to find articles in your field. Abstract The Huajian gold deposit is one of the largest hydrothermal intrusion-related gold deposits in eastern Hebei Province, located in the northern margin of the North China Craton NCC. Introduction The association of mineralization with shoshonitic magmatism is a characteristic feature of the northern part of the North China Craton NCC [ 1 — 4 ]; however, this has not been previously described in detail for Huajian gold deposit Fig 1.
Download: PPT. Fig 1. Regional geological sketch map of the northern part of the North China Craton modified after[ 28 ]. Geological setting and deposit styles Geological setting The Huajian gold deposit is hosted by a Mesozoic-aged volcanic-intrusive complex that forms a part of a larger orogenic belt that is related to the volcanic and associated intrusive rocks that are observed in the northern margin of the NCC Fig 1.
Mineralization styles Mineralization in this deposit comprises quartz vein-type and fracture-zone altered rock. Results and discussion Results Zircon U-Pb age. Fig 5. Major- and Trace-Element geochemistry. Fig 6. Discussion Geochronologic feature of the Mesozoic granitic rocks of the NIC The formation of NCC can be mostly explained by the evolving orogenic processes that span the Precambrian to Mesozoic eras, which were connected to ocean-formation, including subduction and closure, terrain patching, continental collision, and crustal extension [ 2 , 3 , 16 , 18 , 27 , 51 — 58 ].
Fig Trace element discrimination diagram of the tectonic setting after [ 72 ]. Regional tectonic evolution of easten Hebei Province By combining geochemistry with the new age data of the NIC, we infer that easten Hebei Province, which includes the Huajian metallogenic district, was generated in a geodynamic environment controlled by the subduction of the Paleo-Pacific Plate beneath the NCC. Effect of tectonic transformation and potential of polymetallic mineralization The NIC is the pre-eminent example of the connection between hydrothermal-style gold mineralization and shoshonitic magma.
Geochemical characteristics of two dated granites can be distinguished two types. Supporting information. S1 Table. S2 Table. S3 Table. Acknowledgments Thanks are due to Prof. References 1. J Asian Earth Sci. View Article Google Scholar 2. Early Permian plutons from the northern North China Block: constraints on continental arc evolution and convergent margin magmatism related to the Central Asian Orogenic Belt. Int J Earth Sci. View Article Google Scholar 3. Late Paleozoic to Early Mesozoic mafic—ultramafic complexes from the northern North China Block: Constraints on the composition and evolution of the lithospheric mantle.
View Article Google Scholar 4. Pre-Yanshanian geological events in the northern margin of the North China Craton and its adjacent areas.
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Geol China. View Article Google Scholar 5. Ludington S, Plumlee GS. Sillitoe RH. Econ Geol. View Article Google Scholar 7. Mitchell AHG. View Article Google Scholar 8. Metallogeny and tectonics of porphyry copper—molybdenum deposits in British Columbia. Can J Earth Sci. View Article Google Scholar 9. U—Pb zircon and geochemical constraints on the age, origin, and evolution of Paleozoic arc magmas in the Oyu Tolgoi porphyry Cu—Au district, southern Mongolia.