...Figure 3. Cross-valley profile of lower four terraces along Shagou River near Xiaopokou. Strath surfaces are visible beneath all except youngest (T 1 ) terrace. T 4 is displaced by oblique-slip fault and covered with ∼70 m of loess. Soil S 4 at base of T 4 terrace cover formed ca. 425 ka based...

... of the Tibetan Plateau : Tectonics , v. 28 , no. 4 , TC4017 , doi:10.1029/2009TC002455. Pan , B. , Wu , G. , Wang , Y. , Liu , Z. , and Guan , Q. , 2001 , Age and genesis of the Shagou River terraces in eastern Qilian Mountains : Chinese Science Bulletin , v. 46 , no. 6 , p...

... environment of the Longbohe Fe-Cu-(LREE) deposit in the Ailao Shan-Red River shear zone, southwest China: A Neoproterozoic subduction-related IOCG deposit? Lei Liu, Wei Terry Chen, and Xin-Fu Zhao 1 23 Polyphase W-Sn mineralization and rare metal magmatism in relation to the late-Variscan tectono-metamorphic...

... was deposited in a sandy braided river system. Accordingly, the succession from Members 1–2 is the consequence of progradation of fluvial sediments into a lacustrine setting, recording the growth of a delta system. Siltstone and mudstone facies associations in Member 1 might represent prodelta deposits...

... the precipitation ( Jia, 2015 ). Influenced by multiple ice ages, the snowmelt of the Northern Tianshan Mountains easily forms surface runoff and enters the surface water system. Regionally, several rivers developed from west to east ( Figure 1 ), and their discharges change with the seasonal variation...

... Plateau (Figure  1 ), with the Nanshan Mountain to its north, the Ela Mountain and Yellow River Valley to its south, and the Guinan Shagou Guide area to its east ( Yan, 2015 ; Pang et al., 2020 ; Tang et al., 2020 ). The fault binds the basin with the southern margin of the Zongwulong Mountain...

... in the two wings of the Tianbaoshan syncline, including the Xinshan syncline, the Shagou anticline and syncline and the Nangouqing anticline in the Tianbao ore section (Fig.  1 c). Previous studies suggested that the Tianbaoshan area has undergone two episodes of regional compression in nearly NWW–SEE...

... the geometry of the Mishuling pluton aboveground: (1) The northern part of the pluton is relatively higher, and (2) there is no evident change of altitude along the E-W–striking DEM profiles except inflection caused by incision of rivers ( Figs. 11B–11D ). These features define a tear-shape of the Mishuling...

... % NaCl). Finally, Wen et al. ( 2016 ) also provided a simplistic set of physicochemical conditions of formation for Sedex deposits proposing that they formed under reducing conditions, which is characteristic of Selwyn-type Pb–Zn Sedex deposits. Cooke et al. ( 2000 ) recognized the McArthur River...

... by the Huangshui River and its tributaries exposed the Cretaceous to Neogene sequences with numerous index fossils, which have been investigated by many authors (e.g., Horton et al., 2004 ; Dai et al., 2006 ; Dupont-Nivet et al., 2007 ; Abels et al., 2011 ; Hoorn et al., 2012 ; Xiao et al., 2010 , 2012...

... on behalf of the people of the HYC strat- (SEG 1982 F-Lindgren) of South Australia. Before joining the Public Service in iform lead-zinc deposit at McArthur 2002, Paul spent more than 20 years in River, N.T., Australia. This work led to the mining industry in Australia and a growing interest in the use...

.... Canwell prospect drill program on its Forty-seven line km of grid were sur- MAN Cu-Ni-Au-PGE project in the Delta veyed and several anomalies were Teryl Resources Corp. also River district. The drilling efforts were delineated. It is expected that the announced results from limited soil focused on testing...