Sedimentology, sedimentary petrology, and paleoecology of the monsoon-driven, fluvio-lacustrine Zhada Basin, SW-Tibet
In this paper we present sedimentologic, petrographic, and paleoecologic data from a~ 810-
m-thick section of late Neogene (ca. 9–7 to 1Ma) fluvio-lacustrine deposits in the high-
elevation Zhada Basin of SW-Tibet. The tectonic evolution of the Zhada Basin region,
located between the Himalayan Mountains in the S and the Transhimalayan Mountains in
the N, is poorly understood, but sediment accumulation was probably initiated in response to
the middle/late Miocene uplift of the Gurla Mandhata and Leo Pargil domes in the E and W …
m-thick section of late Neogene (ca. 9–7 to 1Ma) fluvio-lacustrine deposits in the high-
elevation Zhada Basin of SW-Tibet. The tectonic evolution of the Zhada Basin region,
located between the Himalayan Mountains in the S and the Transhimalayan Mountains in
the N, is poorly understood, but sediment accumulation was probably initiated in response to
the middle/late Miocene uplift of the Gurla Mandhata and Leo Pargil domes in the E and W …
以上显示的是最相近的搜索结果。 查看全部搜索结果