Macronutrients 发表于 2025-3-28 17:15:27
Ordovician Orogeny and Jurassic Low-Lying Orogen in the Santander Massif, Northern Andes (Colombia)nly of granites and tonalites with a range in ages from 172 to 210 Ma and is interpreted to belong to a low-lying orogen (low-lying Triassic-Jurassic magmatic arc). Present structures in the massif imprint a geometry characterized by converging faults toward the core of the massif giving the appeara花争吵 发表于 2025-3-28 19:58:26
http://reply.papertrans.cn/39/3834/383382/383382_42.pngPeculate 发表于 2025-3-28 23:26:28
Phanerozoic Metallogeny in the Colombian Andes: A Tectono-magmatic Analysis in Space and Time formed in the peri-cratonic or intra-oceanic realm and are allochthonous to the Colombian cordilleras, a result of the complex Meso-Cenozoic accretionary history of the region. Numerous metal deposits and mineral districts are described in detail, and the sympathetic relationship between metal occu委屈 发表于 2025-3-29 03:17:09
http://reply.papertrans.cn/39/3834/383382/383382_44.pngidiopathic 发表于 2025-3-29 09:38:55
Diagnostic Structural Features of NW South America: Structural Cross Sections Based Upon Detailed Findustry, as well as for academic purposes. Most of the sections are balanced or at least admissible. The quality of the presented sections is supported on the coherence among detailed lithologic mapping, lateral facies changes, thickness variations of the lithostratigraphic units, and strict biostra媒介 发表于 2025-3-29 12:58:49
http://reply.papertrans.cn/39/3834/383382/383382_46.png牢骚 发表于 2025-3-29 15:46:14
Exhumation-Denudation History of the Maracaibo Block, Northwestern South America: Insights from Theries. Unraveling the cooling history of the individual blocks leads to an improved understanding of the control of preexisting faults and regional Caribbean geodynamics on the evolution of northwestern South America.路标 发表于 2025-3-29 23:21:24
Diffuse Low-Grade Gliomas in Adultsver was “transferred” to southern Mexico in Late Paleozoic time. Permian magmatic belts running along active margins in Mexico and northern South America place a time limit for this connection at the onset of the assemblage of Pangea.痛恨 发表于 2025-3-30 01:03:45
https://doi.org/10.1007/88-470-0430-6th to the Guajira Peninsula in the north, and continues further northeast into Venezuela and eastwards into the Subandean basins. The Andean basement consists mainly of granulites and other high-grade metamorphic rocks, mainly of supracrustal origin, as well as minor plutons, formed during the Grenvineffectual 发表于 2025-3-30 06:16:03
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