Geologic variation degree-based geochemical exploration anomaly extraction and evaluation method
An evaluation method and variability technology, applied in structured data retrieval, geographic information database, special data processing applications, etc., can solve problems such as few interpolation methods, heavy workload, unclear geological meaning, etc., to reduce costs and risk, the effect of improving accuracy and efficiency
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Embodiment 1
[0033] Example 1: Sichuan Xiasai silver-lead-zinc deposit - one-dimensional soil geochemical profile measurement
[0034] The Xiasai silver-lead-zinc polymetallic deposit is located in the Xiasai-Lianlong tin polymetallic ore concentration area in the north-central section of the Sanjiang metallogenic belt. The river ophiolitic mélange belt is connected to the main arc fold fault belt of Yidun Island arc in the east. The exposed strata in the mining area are mainly the first member of the Triassic Tumugou Formation, which is a set of neritic-littoral neritic clastic sedimentary rocks, which can be subdivided into Five lithological sub-members: the first sub-member is dominated by medium-thick layered feldspar-quartz sandstone; the second sub-member is composed of thin-medium-thick layered medium-grained quartz meta-sandstone, sericite slate, carbonaceous slate rock composition; the main lithology of the third sub-member is tuffaceous feldspar-quartz sandstone interbedded with...
Embodiment 2
[0048] Example 2: Colorful area of Qinghai - two-dimensional washed sediment geochemical scanning survey
[0049] This area is located in the northern section of the Sanjiang giant polymetallic metallogenic belt in southwest China, and is a newly discovered copper polymetallic mineral resource base in recent years ( Figure 6 ). The tectonic location is located on the south side of the Ganzi-Litang suture zone (Chachong ophiolitic mélange) and the northern margin of the North Qiangtang block. The outcropping strata in the area include Mesoproterozoic Ningduo Rock Group, Middle-Late Triassic Bayan Harshan Group, Late Triassic Jiezha Group and Batang Group, and Cenozoic strata. The volcanic ash rock formation of the Batang Group and the Jiapila Formation of the Jieza Group are the main ore-hosting formations in the area.
[0050] The magmatic activity in the area is intense and spans a long time. It has been active from the Indosinian period to the Himalayan period, and the ...
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