Geodetic measurements on behalf of the LGRB identified two uplift areas.
In each of the four uplift events, the mean coseismic uplift is estimated to have been 1.1 1.5 m (Fig. 6).
The topography of Greenland, prior to these uplift events is reconstructed from the present-day, isostatically compensated bedrock by mapping the two main steps in the landscape that resulted from the two uplift phases.
However, as with the other two uplift phases that affected the HTP at ca. 40 35 Ma and 15 10 Ma, paleoclimatic data are still insufficient to clearly demonstrate this linkage.
Even though some of the He ages might reflect a cooling from the temperatures at which He ages partially reset, it is likely that the cooling was derived from one of the three uplift stages.
On the basis of sedimentary facies analyses, three uplift stages were identified in the OBR as (1) surface uplift and regional unconformity (12 9 Ma), (2) differential uplift and compression (6.5 3 Ma), and (3) uplift and intense compression (after ~3 Ma) (Nakajima et al. 2006; Nakajima 2012, 2013).
Family carer burden will be measured by the Uplift/Burden Scale [ 41], a 23-item scale that has six uplift and 17 burden items.
Seven uplifts (Patcham, Khadir, Bela, Chorar, Wagad, Kachchh Mainland, and Saurashtra) occur in three sub parallel trending E W lines.
We applied a characteristic earthquake model to reconstruct the source fault for the four uplift-inducing earthquakes.
Baiyun Depression experienced three evolving formation stages, which are rift stage, thermal subsidence stage and neotectonic stage in the Cenozoic (Gong and Li [1997]; Zhu et al. [2007]), and formed "three uplifts and two depressions", featuring great terrain fluctuations and sharp gradients.
