CN107729595B - Low-temperature chronology thermal history simulation method and system - Google Patents
Low-temperature chronology thermal history simulation method and system Download PDFInfo
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Abstract
The invention discloses a method and a system for simulating low-temperature chronology thermal history, which comprises the following steps: splitting the fission track age of the mineral and bounding the track length by the fission track of the mineral; combining the fission track age of the mineral and/or the fission track bound track length of the mineral with any data type for thermal history simulation. The invention separates the age and the bound track length by combined simulation, so that the age and the bound track length can be used respectively, the age of the fission track, the bound track length and the fitting degree of other various thermal chronology data are calculated respectively, then the fitting results are put together, and comparison and screening are carried out through uniform acceptable fitting degree or high-precision fitting degree, thus generating the comparative use among any methods and any combination on the basis, avoiding the waste of experimental data and saving the experimental cost.
Description
Technical Field
The invention relates to the technical field of thermal history simulation, in particular to a low-temperature chronology thermal history simulation method and system.
Background
The traditional low-temperature chronology thermal history simulation mainly uses two experimental methods of the age of a fission track and the length of a surrounding track and data result combination to carry out temperature-time history simulation. While obtaining both the age of the fission track and the bound track length data is not an easy task. Obtaining age data requires a long experimental period and high experimental cost; obtaining the bounding track length data typically requires a large number of mineral particles. According to the existing thermal history simulation method, one of the two data is unavailable. This leaves a large amount of experimental data idle or sampled samples that do not meet thermal history simulation requirements.
Disclosure of Invention
The present invention is directed to solving, at least to some extent, one of the technical problems in the related art described above.
To this end, it is an object of the present invention to provide a method for simulating a low-temperature chronology thermal history. The low-temperature dating thermal history simulation method splits the combined simulation of the age and the surrounding track length, enables the age and the surrounding track length to be used respectively, calculates the fissile track age, the surrounding track length and the fitting degree of other various thermal dating data respectively, then puts all the fitting results together, and compares and screens the fissile track age, the surrounding track length and the other various thermal dating data through uniform acceptable fitting degree or high-precision fitting degree, so that the comparable use of any method and any combination based on the method are generated, the waste of experimental data is avoided, and the experimental cost is saved.
It is another object of the present invention to provide a low temperature chronology thermal history simulation system.
In order to achieve the above object, the present invention discloses a method for simulating a low-temperature chronology thermal history, comprising: splitting the fission track age of the mineral and bounding the track length by the fission track of the mineral; combining the fission track age of the mineral and/or the fission track bound track length of the mineral with any data type for thermal history simulation.
According to the low-temperature dating thermal history simulation method, the age and the surrounding track length are jointly simulated and split, so that the age and the surrounding track length can be used respectively, the fissile track age, the surrounding track length and the fitting degree of various other thermal history data are calculated respectively, then the fitting results are put together, and comparison and screening are performed through uniform acceptable fitting degree or high-precision fitting degree, so that the comparison and use among any methods and any combination based on the method are generated, the waste of experimental data is avoided, and the experimental cost is saved.
In addition, the method for simulating the low-temperature chronological thermal history according to the above embodiment of the present invention may also have the following additional technical features:
further, combining the fission track age of the mineral with any data type to perform thermal history simulation, specifically comprising: combining one or more of the fission track age of the minerals, the U-Th/He age of the minerals, the fission track surrounding track length of the minerals, the Ar-Ar age of mica, the vitrinite reflectivity and the light-releasing method of the quartz of the bedrock to carry out thermal history simulation; or combining the fission track surrounding track length of the mineral with one or more of the U-Th/He age of the mineral, the fission track age of the mineral, the Ar-Ar age of mica, the vitrinite reflectivity and the light-release method of the quartz of the bedrock to carry out thermal history simulation.
In another aspect of the invention, a low temperature chronology thermal history simulation system is disclosed, comprising: the splitting module is used for splitting the fission track age and the fission track bound track length of the mineral; and the thermal history simulation module is used for combining the fission track age of the mineral and/or the fission track surrounding track length of the mineral with any data type to perform thermal history simulation.
According to the low-temperature dating thermal history simulation system, the age and the surrounding track length are jointly simulated and split, so that the age and the surrounding track length can be used respectively, the fissile track age, the surrounding track length and the fitting degree of various other thermal history data are calculated respectively, then the fitting results are put together, and comparison and screening are performed through uniform acceptable fitting degree or high-precision fitting degree, so that the comparison and use among any methods and any combination based on the method are generated, the waste of experimental data is avoided, and the experimental cost is saved.
In addition, the low-temperature chronology thermal history simulation system according to the above embodiment of the present invention may also have the following additional technical features:
further, the thermal history simulation module is used for combining the fission track age of the minerals with one or more of the U-Th/He age of the minerals, the fission track surrounding track length of the minerals, the Ar-Ar age of mica, the reflectivity of vitrinite and the quartz light-release method of bedrock to carry out thermal history simulation; or combining the fission track surrounding track length of the mineral with one or more of the U-Th/He age of the mineral, the fission track age of the mineral, the Ar-Ar age of mica, the vitrinite reflectivity and the light-release method of the quartz of the bedrock to carry out thermal history simulation.
Further, still include: and the display module is used for displaying the thermal history simulation result.
Additional aspects and advantages of the invention will be set forth in part in the description which follows and, in part, will be obvious from the description, or may be learned by practice of the invention.
Drawings
The above and/or additional aspects and advantages of the present invention will become apparent and readily appreciated from the following description of the embodiments, taken in conjunction with the accompanying drawings of which:
FIG. 1 is a flow diagram of a method of low temperature chronological thermal history simulation according to one embodiment of the present invention;
FIG. 2 is a schematic diagram of a thermal history simulation data type combination selection;
FIG. 3 is a schematic representation of the selection of apatite fission track age in combination with apatite U-Th/He age;
FIG. 4 is a graphical representation of apatite fission track age combined with apatite U-Th/He age input data;
FIG. 5 is a default display interface of apatite fission track age combined with apatite U-Th/He age simulation results;
FIG. 6 is a conventional display interface of apatite fission track age combined with apatite U-Th/He age simulation results;
FIG. 7 is a schematic representation of a combined selection of zircon fission track age, apatite fission track age, mica Ar-Ar age;
FIG. 8 is a graphical representation of combined input data for zircon fission track age, apatite fission track age, mica Ar-Ar age;
FIG. 9 is a default display interface of zircon fission track age, apatite fission track age, mica Ar-Ar age combination simulation results;
FIG. 10 is a conventional display interface of zircon fission track age, apatite fission track age, mica Ar-Ar age combination simulation results;
FIG. 11 is a schematic representation of a selection of a vitrinite reflectance in combination with an apatite fission trace bounding trace length;
FIG. 12 is a graphical illustration of input data combining vitrinite reflectance and apatite fission trace bounding trace length;
FIG. 13 is a default display interface of a simulation result of a vitrinite reflectance combined with an apatite fission trace bounding trace length;
FIG. 14 is a conventional display interface of the combined simulation results of vitrinite reflectance and apatite fission trace bounding trace length;
FIG. 15 is a block diagram of a low temperature chronology thermal history simulation system according to one embodiment of the present invention.
Detailed Description
Reference will now be made in detail to embodiments of the present invention, examples of which are illustrated in the accompanying drawings, wherein like or similar reference numerals refer to the same or similar elements or elements having the same or similar function throughout. The embodiments described below with reference to the accompanying drawings are illustrative only for the purpose of explaining the present invention, and are not to be construed as limiting the present invention.
The method and system for simulating the thermal history of the low-temperature era according to the embodiment of the invention are described in the following with reference to the attached drawings.
FIG. 1 is a flow chart of a method of low temperature chronological thermal history simulation according to one embodiment of the present invention.
As shown in FIG. 1, a method for low temperature annual thermal history simulation according to one embodiment of the present invention comprises:
s110: the fission track age of the split mineral and the fission track bounding track length of the mineral.
Particularly, the acquisition of the fission track age of the mineral and the fission track bound track length of the mineral is not easy, the acquisition time period is long, and the experiment cost is high, so that the binding of the fission track age of the mineral and the fission track bound track length of the mineral can be disassembled, the experiment cost can be saved, the experiment period can be shortened, the experiment data can be developed and utilized as much as possible, and the idle and waste of the experiment data are effectively avoided.
S120: a thermal history simulation is performed combining the fission track age of a mineral and/or the fission track bound track length of the mineral with any data type.
The method specifically comprises the following steps: combining one or more of the fission track age of the minerals, the U-Th/He age of the minerals, the fission track surrounding track length of the minerals, the Ar-Ar age of mica, the vitrinite reflectivity and the light-releasing method of the quartz of the bedrock to carry out thermal history simulation; or combining the fission track surrounding track length of the mineral with one or more of the U-Th/He age of the mineral, the fission track age of the mineral, the Ar-Ar age of mica, the vitrinite reflectivity and the light-release method of the quartz of the bedrock to carry out thermal history simulation.
In particular, the mineral's fission track age and/or the mineral's fission track bound track length may be combined with any data type, two data type combinations, three data type combinations, or more data type combinations. As shown in FIG. 2, the embodiment of the present application can be implemented by a Low-T Thermo software. When the software is used, the data type input interface comprises the following steps: apatite Fission Track Age (Apatite Fission Track Age), Apatite U-Th/He (Apatite U-Th/He), Zircon Fission Track Age (zirconia Fission Track Age), Mica Ar-Ar Age (Mica Ar-Ar), vitrinite reflectance (% Ro), Apatite Fission Track bound Track Length (Apatite Fission Track Length), Zircon U-Th/He (zirconia U-Th/He), and Bedrock Quartz luminescence (Bedrop Quartz OSL), the software can realize 255 combinations in total, wherein single data type is used, thereby greatly increasing the selection of simulation combinations.
As shown in fig. 3, the corresponding Apatite Fission Track Age (Apatite fistion Track Age) and the Apatite U-Th/He Age (Apatite U-Th/He Age) are selected and combined to perform the thermal history simulation, and as shown in fig. 4, the corresponding data types are input, and the Apatite U-Th/He Age has the options Using mean (average Age) and Using multiple (multiple ages), in this example, the Using multiple data input is selected, and the Apatite fistion Track Age has the options Age and sigma (standard error), and the two data are selected and input. In conjunction with FIG. 5, the software of the present application further includes a data results display, wherein the interface for default display of results, C1 represents simulated results, and wherein the thermal history curves are all acceptable thermal history curves, and wherein the black bold line (i.e., the average thermal history curve) represents the optimal thermal history simulation results. The corresponding eU (effective uranium concentration) versus Age (Age value) graph and the Age value corresponding to the optimal thermal history simulation curve (black bold line in the simulation results) are shown on the right. Referring to FIG. 6, in the conventional display style, C2 represents the final simulation result, the gray-white part range P1 is the acceptable range, and the gray-black part range P2 is the high precision range (GOF ≧ 0.5, where GOF represents the deviation degree of the simulation value from the experimental measured value). Wherein the black bold line (i.e., the average thermal history curve) represents the optimal thermal history simulation results. The corresponding eU (effective uranium concentration) versus Age (Age value) graph and the Age value corresponding to the optimal thermal history simulation curve (black bold line in the simulation results) are shown on the right.
Take three combinations as an example: a thermal history simulation was performed by combining the Age of a Zircon Fission Track (Zircon fusion Track Age), the Age of an Apatite Fission Track (Apatite fusion Track Age), and the Age of Mica Ar-Ar (Mica Ar-Ar).
As shown in fig. 7, the combination of the corresponding Zircon Fission Track Age (zirconia Fission Track Age), Apatite Fission Track Age (apatate Fission Track Age), and Mica Ar-Ar Age (Mica Ar-Ar) was selected and subjected to the thermal history simulation, and as shown in fig. 8, the corresponding data type was input, and for apatate Fission Track Age, the options Age and σ (standard error) were input, and for Zircon Fission Track Age, the corresponding options Age and σ (standard error) were input, and for Mica Ar-Ar, the corresponding options Age and σ (standard error) were input, the corresponding options Age and σ (standard error), Ea (activation energy), D0 (diffusion coefficient at infinite high temperature), and Tc (sealing temperature). In conjunction with FIG. 9, the software of the present application further includes a data results display, wherein the interface for default display of results, C3 represents simulated results, and wherein the thermal history curves are all acceptable thermal history curves, and wherein the black bold line (i.e., the average thermal history curve) represents the optimal thermal history simulation results. The age values for the optimal thermal history simulation curve (black bold line in the simulation results) are shown on the right. Referring to FIG. 10, in the conventional display style, C4 represents the final simulation result, the gray-white part range P1 is the acceptable range, and the gray-black part range P2 is the high precision range (GOF ≧ 0.5, where GOF represents the deviation degree of the simulation value from the experimental measured value). Wherein the black bold line (i.e., the average thermal history curve) represents the optimal thermal history simulation results. The age values for the optimal thermal history simulation curve (black bold line in the simulation results) are shown on the right.
In conjunction with 11, a thermal history simulation was performed by combining the Apatite Fission Track Length (Apatite fusion Track Length) and the vitrinite reflectance (% Ro). The corresponding data types are input as shown in fig. 12, wherein the input data in% Ro are% Ro (vitrinite reflectance), σ (standard error), stratgraphic Age, Calibration (Calibration mode), and the input data Length (Length) and Angle to C-axis (Angle between the bounding path and the mineral C axis) in the Apatite Fission Track Length. In conjunction with FIG. 13, the software of the present application further includes a data results display, wherein the interface displaying the results, C5 represents the simulated results, and the thermal history curves in the graph are all acceptable thermal history curves, wherein the black bold line (i.e., the average thermal history curve) represents the optimal thermal history simulation results. The corresponding apatite fission track bounding track length distribution map and the age value corresponding to the optimal thermal history simulation curve (black bold line in the simulation result) are shown on the right. Referring to FIG. 14, in the conventional display style, C6 represents the final simulation result, the gray-white part range P1 is the acceptable range, and the gray-black part range P2 is the high precision range (GOF ≧ 0.5, where GOF represents the deviation degree of the simulation value from the experimental measured value). Wherein the black bold line (i.e., the average thermal history curve) represents the optimal thermal history simulation results. The corresponding apatite fission track bounding track length distribution map and the age value corresponding to the optimal thermal history simulation curve (black bold line in the simulation result) are shown on the right.
According to the low-temperature dating thermal history simulation method, the age and the surrounding track length are jointly simulated and split, so that the age and the surrounding track length can be used respectively, the fissile track age, the surrounding track length and the fitting degree of various other thermal history data are calculated respectively, then the fitting results are put together, and comparison and screening are performed through uniform acceptable fitting degree or high-precision fitting degree, so that the comparison and use among any methods and any combination based on the method are generated, the waste of experimental data is avoided, and the experimental cost is saved.
FIG. 15 is a block diagram of a low temperature chronology thermal history simulation system according to one embodiment of the present invention.
As shown in FIG. 15, a low temperature annual thermal history simulation system 200 according to one embodiment of the present invention comprises: a splitting module 210 and a thermal history modeling module 220.
Wherein the splitting module 210 is configured to split the fission track age and the fission track bound track length of the mineral. The thermal history simulation module 220 is used to perform thermal history simulation combining the fission track age of a mineral and/or the fission track envelope track length of the mineral with any data type.
According to the low-temperature dating thermal history simulation system, the age and the surrounding track length are jointly simulated and split, so that the age and the surrounding track length can be used respectively, the fissile track age, the surrounding track length and the fitting degree of various other thermal history data are calculated respectively, then the fitting results are put together, and comparison and screening are performed through uniform acceptable fitting degree or high-precision fitting degree, so that the comparison and use among any methods and any combination based on the method are generated, the waste of experimental data is avoided, and the experimental cost is saved.
In some embodiments, the thermal history simulation module 220 is configured to combine the fission track age of the mineral with one or more of the U-Th/He age of the mineral, the fission track perimeter track length of the mineral, the Ar-Ar age of mica, the reflectivity of vitrinites, and the quartz photoluminescence method of bedrock to perform thermal history simulation; or combining the fission track surrounding track length of the mineral with one or more of the U-Th/He age of the mineral, the fission track age of the mineral, the Ar-Ar age of mica, the vitrinite reflectivity and the light-release method of the quartz of the bedrock to carry out thermal history simulation.
In some embodiments, further comprising: and the display module is used for displaying the thermal history simulation result.
It should be noted that a specific implementation manner of the low-temperature chronology thermal history simulation system according to the embodiment of the present invention is similar to a specific implementation manner of the low-temperature chronology thermal history simulation method according to the embodiment of the present invention, and please refer to the description of the low-temperature chronology thermal history simulation method part, which is not repeated herein in order to reduce redundancy.
Furthermore, the terms "first", "second" and "first" are used for descriptive purposes only and are not to be construed as indicating or implying relative importance or implicitly indicating the number of technical features indicated. Thus, a feature defined as "first" or "second" may explicitly or implicitly include at least one such feature. In the description of the present invention, "a plurality" means at least two, e.g., two, three, etc., unless specifically limited otherwise.
In the present invention, unless otherwise expressly stated or limited, the terms "mounted," "connected," "secured," and the like are to be construed broadly and can, for example, be fixedly connected, detachably connected, or integrally formed; can be mechanically or electrically connected; they may be directly connected or indirectly connected through intervening media, or they may be connected internally or in any other suitable relationship, unless expressly stated otherwise. The specific meanings of the above terms in the present invention can be understood by those skilled in the art according to specific situations.
In the description herein, references to the description of the term "one embodiment," "some embodiments," "an example," "a specific example," or "some examples," etc., mean that a particular feature, structure, material, or characteristic described in connection with the embodiment or example is included in at least one embodiment or example of the invention. In this specification, the schematic representations of the terms used above are not necessarily intended to refer to the same embodiment or example. Furthermore, the particular features, structures, materials, or characteristics described may be combined in any suitable manner in any one or more embodiments or examples. Furthermore, various embodiments or examples and features of different embodiments or examples described in this specification can be combined and combined by one skilled in the art without contradiction.
Although embodiments of the present invention have been shown and described above, it is understood that the above embodiments are exemplary and should not be construed as limiting the present invention, and that variations, modifications, substitutions and alterations can be made to the above embodiments by those of ordinary skill in the art within the scope of the present invention.
Claims (3)
1. A method for simulating a low-temperature chronology thermal history is characterized by comprising the following steps:
splitting the fission track age of the mineral and bounding the track length by the fission track of the mineral;
combining the age of the fission track of the mineral and/or the length of the fission track bound track of the mineral with any data type to perform thermal history simulation, wherein the thermal history simulation specifically comprises the following steps: combining one or more of the fission track age of the minerals, the U-Th/He age of the minerals, the fission track surrounding track length of the minerals, the Ar-Ar age of mica, the vitrinite reflectivity and the light-releasing method of the quartz of the bedrock to carry out thermal history simulation; or combining the fission track surrounding track length of the mineral with one or more of the U-Th/He age of the mineral, the fission track age of the mineral, the Ar-Ar age of mica, the vitrinite reflectivity and the light-releasing method of the quartz of the bedrock to carry out thermal history simulation;
the mineral U-Th/He age comprises mineral U-Th/He average age data and mineral U-Th/He multiple age data, the mineral fission track age comprises standard error data, and the mineral fission track bounding track length comprises data of an included angle between a bounding track and a mineral C axis.
2. A low-temperature chronology thermal history simulation system, comprising:
the splitting module is used for splitting the fission track age and the fission track bound track length of the mineral;
the thermal history simulation module is used for combining the fission track age of the mineral and/or the fission track peripheral track length of the mineral with any data type to perform thermal history simulation, and is specifically used for combining the fission track age of the mineral with one or more of the U-Th/He age of the mineral, the fission track peripheral track length of the mineral, the Ar-Ar age of mica, the vitrinite reflectivity and the quartz light-release method of the bedrock to perform thermal history simulation; or combining the fission track surrounding track length of the mineral with one or more of the U-Th/He age of the mineral, the fission track age of the mineral, the Ar-Ar age of mica, the vitrinite reflectivity and the light-releasing method of the quartz of the bedrock to carry out thermal history simulation;
the mineral U-Th/He age comprises mineral U-Th/He average age data and mineral U-Th/He multiple age data, the mineral fission track age comprises standard error data, and the mineral fission track bounding track length comprises data of an included angle between a bounding track and a mineral C axis.
3. The low temperature annual thermal history simulation system of claim 2, further comprising: and the display module is used for displaying the thermal history simulation result.
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| CN110390120B (en) * | 2018-04-23 | 2022-11-25 | 中山大学 | Method and system for simulating chronology thermal history of basement rock quartz light-release |
| CN109100484B (en) * | 2018-07-31 | 2020-08-04 | 成都理工大学 | Hydrocarbon generation history research method under thermal history and hydrocarbon generation thermal simulation constraints |
| CN109115732B (en) * | 2018-08-02 | 2021-07-13 | 华南理工大学广州学院 | Sensitivity correction method for photoluminescence yearly experiment |
| CN112685909B (en) * | 2021-01-08 | 2023-11-14 | 中山大学 | Thermal history simulation method and device based on age of multiparticulate U-Th/He |
| CN113076651B (en) * | 2021-04-12 | 2023-05-12 | 中山大学 | Method and related device for recovering bedrock stripping history based on universe causative nuclide |
| CN113722917B (en) * | 2021-09-01 | 2023-08-22 | 中山大学 | Thermal history simulation method and system based on fissile track length distribution on vertical section |
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