How gold mineral deposits in ghana related to tectonics?4 answersGold mineral deposits in Ghana are intricately related to tectonic processes. In the Bogosu-Prestea mining district, gold precipitation occurred within sulphide/arsenide minerals due to metamorphic/hydrothermal gradients, host mineral properties, and post-depositional deformation. At Damang, gold mineralization is associated with hydrothermal sheeted quartz veins formed by metamorphic fluids from devolatisation reactions in greenstones, indicating an orogenic lode gold mineralization process. In the Kyerano area, NE-SW and NNW-SSE trending regional structures, associated with tectonic episodes, control gold mineralization by localizing it along major fracture systems. The Lawra Belt's metavolcanic rocks and enclaves formed in an island-arc setting through subduction-related magmatism, highlighting the tectonic control on gold mineralization in the region. The hydrothermal system in the Ashanti gold belt experienced episodic fluid expulsion and phase separation, leading to gold precipitation at relatively high crustal levels due to tectonic processes.
What is the tectonic setting of the Salt Range?4 answersThe tectonic setting of the Salt Range is mainly characterized by Oceanic and Continental Island arcs as well as Active Continental margin. The structural changes across the Salt Range area reflect a systematic variation in the stage of their tectonic development. The Salt Range is an active participant in the southward migration of the Himalayan thrust front. The tectonic features in the Salt Range include thrust, normal, and reverse faults, which are influenced by the distribution of the thick salt sequence. The integration of seismic reflection data and surface geologic data has helped in delineating different tectonic features in the Salt Range, including a concealed duplex structure and variations in the deformational style within the leading edge.
What is the geological history of the Red Sea?5 answersThe Red Sea has undergone significant geological evolution. The rift began in the Late Oligocene, with extension and rifting initiating in the southern Red Sea and later in the northern Red Sea. The rift structure was complex, with distinct sub-basins and alternating regional dip domains separated by accommodation zones. Sedimentary facies were dominated by siliciclastics, and neotethyan faunas appeared. In the Early Burdigalian, tectonically-driven subsidence accelerated, resulting in increased denudation and uplift of the rift shoulders. The Middle Miocene saw a switch from orthogonal to oblique rifting and the development of an extensive evaporitic basin. Seafloor spreading in the southern Red Sea began in the earliest Pliocene, re-establishing open marine conditions. Pleistocene sea-level changes led to the formation of coral terraces and wave-cut benches. The lithological distribution in the Red Sea is mainly comprised of limestones, evaporites, and shales, with the evaporite body representing a significant portion of the succession. Syn-rift faulting and rifting played a prominent role in shaping the basin's stratigraphic evolution.
What is the geological history of the Sinai Peninsula?5 answersThe geological history of the Sinai Peninsula spans over a time span of approximately 450 million years. It is characterized by a complex history of magmatism, sedimentation, and metamorphism. The Precambrian basement of the Sinai Peninsula records three main magmatic age populations at 1025-975 Ma, 850-725 Ma, and 650-575 Ma, representing volcanic arc magmatic episodes. The region also experienced post-collisional within-plate alkaline-peralkaline magmatism at the end of the Neoproterozoic time. The basement rocks of the Sinai Peninsula have undergone multiple metamorphic events, with high-grade metamorphism occurring at 800-750 Ma and 627-592 Ma in the Kid and Feiran-Solaf metamorphic complexes, respectively. The tectonic evolution of the Sinai Peninsula can be divided into five stages, including the Rodinia breakup, formation of volcanic arcs, arc-arc collision, escape tectonics, and lithospheric delamination. The region has also been influenced by major tectonic events such as the opening of the Tethys, the Syrian arc system, the Gulf of Suez rifted basin, and the Dead Sea-Gulf of Aqaba rift.
What is the text of "On the Red Sea"?4 answers"On the Red Sea" is a Peripatetic treatise on the marine fauna of the Red Sea, likely based on first-hand research conducted at a Ptolemaic settlement in the northern Red Sea. It is argued that this treatise was known to at least one later Alexandrian lexicographer and may have been accessed by Agatharchides of Cnidus in the second century BC. The book "Red Sea—Red Square—Red Thread" explores narratives of emancipation in philosophy, theology, politics, and the arts, using the Red Sea anecdote as a central theme. "On the Red Sea" is also mentioned in a historiographical sketch of Red Sea studies. However, it is important to note that the specific text of "On the Red Sea" is not provided in the abstracts provided.
How far back in time can we see the geological record?5 answersThe geological record can be seen back to about 4.5 billion years ago. This record is based on the observation of rocks that make up the Earth's crust, which provide evidence of the Earth's past evolution. Over the years, advances in stratigraphy and dating techniques have allowed scientists to organize geological time into different intervals, including the Hadean, Archean, Proterozoic, and Phanerozoic Eons. Sedimentary cycles in marine sedimentary archives have also been used to estimate the duration of parts of the geological record, providing evidence that the Earth is much older than previously thought. The discovery of radioactivity helped resolve the debate about the age of the Earth, confirming that it is indeed billions of years old.