...Figure 9 The present and ancient abandoned meandering channels of the lower reach of the Manas river to the north of the northern Tian Shan orogenic wedge (modified after Cui et al. [ 67 ]). R4—the present meandering channel of the lower reach of the Manas River 500 years ago to the present, R3...

... fault; ATF: Altyn Tagh fault; KF: Karakoram fault. (b) Tectonic and topographic map of the northern Chinese Tian Shan with major rivers. Red solid lines show the locations of the Manas and Guertu sampling sections. The area surrounded by reddish dash lines is the location of Figure 2 . F1: northern...

...Fig. 7. (Fe 2 O 3 * + MgO)–TiO 2 ( a ) ( Bhatia, 1983 ) and La–Th–Sc ( b ) ( Bhatia and Crook, 1986 ) discrimination composition diagrams for metamorphic rocks of the Derba block (group II). 1, 2, Alygdzher Formation of the Mana (1) and Uda (2) areas; 3, Zhaima Formation of the Krol River area...

... the subsurface geometry of a highly segmented thrust system in the southern Junggar basin, northwest China, which generated the 1906 M w  7.4–8.2 Manas, China, earthquake ( Avouac et al. , 1993 ; Burchfiel et al. , 1999 ; Wang et al. , 2004 ). This rupture has been interpreted to breach surface‐trace...

... , 155 – 170 . Gong , Z.J. , Li , S.H. , Li , B. , 2014 . The evolution of a terrace sequence along the Manas River in the northern foreland basin of Tian Shan, China, as inferred from optical dating . Geomorphology 213 , 201 – 212...

... that these changes were the main factors influencing sandstone composition. At Manas, Lt-rich, Qt-poor Triassic sandstone deposited by gravelly braided rivers is overlain by Lower and Middle Jurassic meandering-fluvial and lacustrine sandstone containing appreciably greater percentages of Qt and total F and less Lt...

... a series of imbricated fault-related folds. The most prominent fold trend in southern Junggar consists of the Tugulu, Manas, and Huoerguosi anticlines, which trap hydrocarbons in clastic Eocene reservoirs. These structures exhibit complex internal geometries, with coeval forethrusts and backthrusts forming...

... and middle parts (within the Cabora Bassa Rift-basin and the Mana Pools and Mid-Zambezi Basins) of the modern Zambezi River follow the same rift valleys as a major Permo-Triassic (Karoo) lake and river system, which originally flowed westwards across the interior of the (Western) Gondwana Supercontinent...

... of Neoproterozoic deposits (see Fig. 2 ): 1, 2 — northwestern East Sayans (Mana through): 1 — Goryunov ravine, 2 — Mana, Zhistyk, and Ungut Rivers; 3–5 — southeastern East Sayans: 3 — Sarkhoi, Ukha-Gol, and Bokson Rivers, 4 — Sarkhoi and Muya-Gol Rivers, 5 — Gorlyk and Shumak Rivers; 6 — Gornaya Shoria, Mrassu...

... . They ubiquitously form bioherm strata of the Koril Member. A bioherm composed of Renalcis polymorphus lies 12 m below, and, at the Bol’shaya Kuonamka River, Renalcis sp. was found in the underlying Staraya Rechka Formation (50 m below the roof). In the Igarka region, at the Sukharikha River (northwestern...

..., nephelinitic, melilititic and carbonatite magmatism ranging in age from c . 5.9 Ma (Mana et al . 2015 ) to the current activity in the Oldoinyo Lengai area (Dawson, 2008 ; Reiss et al . 2021 ). Fig. 1. Locations of the major volcanoes in the North Tanzanian Divergence discussed in this work (after...

... processes by the Mana Plain ( Fig. 2 ), and the abandoned sea cliffs have 30–40-m-tall talus piles near their base. Previous cosmogenic 3 He exposure dating of the abandoned sea cliffs just north of Ka’ula’ula Valley returned ages up to 30 ka ( Mukhopadhyay et al., 2003 ), suggesting minimal cliff erosion...