阅读说明：本技术 一种隐伏沉积型富锰矿识别方法 (Hidden deposition type manganese-rich ore identification method ) 是由 高永宝 滕家欣 贺永康 陈登辉 隋清霖 于 2019-09-24 设计创作，主要内容包括：本发明提供了一种隐伏沉积型富锰矿识别方法,包括如下步骤：步骤1,通过井中激发极化法激电测量圈定极化率在矿体位置的异常变化；步骤2,通过井中激发极化法激电测量圈定极化率在非矿位置的异常变化；步骤3,通过圈定极化率在矿体位置和非矿位置的异常变化推测富矿体延伸情况,进而识别隐伏沉积型富锰矿。步骤1和步骤2的井中激发极化法激电测量包括地-井工作方式、井-地工作方式和井-井工作方式。通过井中激发极化法进行激电测量,圈定极化率在矿体位置与非矿位置的异常变化推测富矿体延伸情况,通过在矿体激发电场能够更有效的识别深部锰矿体的延伸方向。(The invention provides a method for identifying a hidden sedimentary manganese-rich ore, which comprises the following steps: step 1, measuring abnormal change of enclosed polarizability at the position of an ore body by induced polarization in a well; step 2, measuring abnormal change of the delineation polarizability at a non-mine position by induced polarization in a well; and 3, inferring the extension condition of the ore-enriched body by delineating the abnormal changes of the polarizability at the position of the ore body and the position of the non-ore body, and further identifying the hidden sedimentary manganese-enriched ore. The induced polarization method induced polarization measurement in the well in the step 1 and the step 2 comprises an earth-well working mode, a well-earth working mode and a well-well working mode. The method is characterized in that induced polarization measurement is carried out through an in-well induced polarization method, the abnormal change of polarizability at ore body positions and non-ore positions is determined to infer the ore body extending condition, and the extending direction of the deep manganese ore body can be more effectively identified through an ore body excitation power field.)

1. The method for identifying the blind sedimentary manganese-rich ore is characterized by comprising the following steps of:

step 1, measuring abnormal change of enclosed polarizability at the position of an ore body by induced polarization in a well;

step 2, measuring abnormal change of the delineation polarizability at a non-mine position by induced polarization in a well;

and 3, inferring the extension condition of the ore-enriched body by delineating the abnormal changes of the polarizability at the position of the ore body and the position of the non-ore body, and further identifying the hidden sedimentary manganese-enriched ore.

2. The method for identifying the lateritic deposit type manganese-rich ore according to claim 1, wherein: the induced polarization method induced polarization measurement in the well of the step 1 and the step 2 comprises an earth-well working mode, a well-earth working mode and a well-well working mode.

3. The method for identifying the lateritic sedimentary manganese-rich ore according to claim 2, wherein the earth-well operation mode includes two arrangements: one is to use a metal casing as a power supply electrode A, namely, a wellhead grounding ground-well mode can be used for finding out blind mines at the bottom of a well and determining a background value; another method is to place a at r from the well head and change its orientation to the borehole, make primary and secondary induced polarization measurements in the well for each different a pole orientation, called earth-well mode orientation measurements, for ascertaining the well-side blind mine and determining its spatial location, and earth-well mode operation for ascertaining the well-side blind mine and determining its spatial location, ascertaining the well-bottom blind mine, determining the background value.

4. The method for identifying the lateritic deposit type manganese-rich ore according to claim 2, wherein: well-to-ground operating modes are divided into well-to-ground profile measurements and well-to-ground laser depths.

5. The method for identifying the lateritic deposit type manganese-rich ore according to claim 4, wherein: the well-local profile measurement comprises: the electrode is placed at a selected depth in the well, the other electrode is arranged on the ground at infinity, and the measuring electrode MN is arranged on the ground and measures along a measuring line, including cross section and longitudinal section measurement and vector measurement.

6. The method for identifying the lateritic deposit type manganese-rich ore according to claim 4, wherein: the well-local induced electrical sounding comprises: the method comprises the steps of placing a power supply electrode in a well, enabling the other electrode to be located on the ground at infinity, changing the depth of the power supply electrode point by point, fixing measuring electrodes M and N to a well mouth for observation at a certain distance, and enabling the well-local induced polarization depth measurement to be used for tracking the trend of an ore body and judging the occurrence factor of the ore body.

7. The method for identifying the lateritic deposit type manganese-rich ore according to claim 2, wherein: the well-to-well arrangement device is divided into 2 types: the single well-well mode and the double well-well mode place the power supply device and the measuring device in the same borehole, and comprise induced polarization logging and intermediate gradient in the single well; in the twin-well method, the power supply device is placed in one borehole, and the measuring device is placed in the other borehole, so that work can be performed only by simultaneously having two boreholes.

8. The method for identifying the lateritic deposit type manganese-rich ore according to claim 7, wherein: the induced polarization logging is used for dividing a drilling geological profile and determining induced electrical property parameters.

9. The method for identifying the lateritic deposit type manganese-rich ore according to claim 1, wherein: the well-to-well induced well-to-well electrical stimulation curve generated by the well-to-well method comprises:

(1) unipolar fixed power supply arrangement: generating big upper, right and lower negative exceptions, wherein the position of the zero value point corresponds to the burial depth of the right end of the ore body;

(2) intermediate gradient arrangement: the curve amplitude is not large, and the position of the maximum value corresponds to the burial depth of the right end of the ore body;

(3) bipolar synchronous alignment: the curve amplitude is large, and the position of the maximum value corresponds to the buried depth of the right end of the ore body.

Technical Field

The invention relates to a geophysical exploration and information technology method in the geological mineral exploration field, in particular to a hidden sedimentary manganese-rich ore identification method.

Background

The 80 s of China found 3 types of manganese-rich ores, namely marine sedimentary type, sedimentary metamorphic type and weathering type, wherein the latter can be further divided into two subclasses of ancient weathering type and modern weathering type. Marine sedimentary manganese ore has been found in recent years to be of a medium size deposit. The industrial type of ore belongs to a complex manganese ore with low phosphorus, low iron and low silicon. The sedimentary metamorphic manganese ore is added in a set of marine process of changing clastic rock into argillaceous limestone in a certain place, and due to the influence of late hydrothermal metamorphism, the ore contains manganese carbonate ore and manganese carbonate-manganite ore. The latter also contains a certain amount of rosepsite, accompanied by sulfides such as galena, sphalerite, pyrite and the like. The modern weathered ore deposit is formed by exposing various cause types of dreams or manganese-containing rock series to the ground surface, enriching the dreams or the manganese-containing rock series in a fourth red layer of an oxidation zone through weathered leaching, has a manganese cap type, a leaching type and a stacking type, and is the most one type found in the complex manganese ore at present. Because the sedimentary manganese ore body is influenced by later-stage modification, the local exposure of the manganese ore body and the extension of the manganese ore body in deep and peripheral hidden areas are major geological problems restricting the prospecting. Meanwhile, the deposited manganese ore has the characteristics of stable and continuous layer positions, is closely related to organic matters, has stronger reduction effect on the organic matters, is an important mechanism for forming the manganese-rich ore, and has higher organic matter content at the manganese-containing layer position.

The traditional identification method for the sedimentary manganese ore mainly utilizes earth surface outcrop observation, magnetic measurement and ground excitation work to determine abnormity. Such as: earth outcrop observation employs visual inspection to look for outcrops or to delineate manganese ore bodies by identification of their surrounding rocks and identification of structural markers. The common method for delineating the manganese ore body through the magnetic measurement of the geophysical exploration technology and the ground induced polarization work is generally to identify weak positive anomaly or positive and negative anomaly boundary of the magnetic measurement; and high polarization characteristics of the induced current.

The existing method has certain limitations, such as: the earth surface outcrop observation method cannot be applied if a certain coverage stratum exists; the precondition for determining the ore body through magnetic measurement is that a manganese ore body is formed and simultaneously a large amount of magnetite is associated, and if the content of the magnetite is low, the ore body cannot be effectively identified through the magnetic measurement method; in ground power excitation work, due to the fact that the depth of the buried depth of an ore body is increased, power excitation caused by metal sulfides accompanying a manganese ore body is quite weak, and the ore body buried deep cannot be effectively detected by the ground power excitation work.

Disclosure of Invention

In order to overcome the defects of the prior art, the invention aims to carry out induced polarization measurement by an in-well induced polarization method, and determine the abnormal change of the polarizability at the position of an ore body and the position of a non-ore body to infer the ore body-rich extension condition. The extending direction of the deep manganese ore body can be more effectively identified through the ore body excitation power field.

The invention aims to provide a method for identifying a hidden sedimentary manganese-rich ore, which comprises the following steps:

step 1, measuring abnormal change of enclosed polarizability at the position of an ore body by induced polarization in a well;

step 2, measuring abnormal change of the delineation polarizability at a non-mine position by induced polarization in a well;

and 3, inferring the extension condition of the ore-enriched body by delineating the abnormal changes of the polarizability at the position of the ore body and the position of the non-ore body, and further identifying the hidden sedimentary manganese-enriched ore.

Preferably, the induced polarization method induced polarization measurement in the well of the step 1 and the step 2 comprises a ground-well operation mode, a well-ground operation mode and a well-well operation mode.

Preferably, the earth-well mode of operation comprises two permutations: one is to use a metal casing as a power supply electrode A, namely, a wellhead grounding ground-well mode can be used for finding out blind mines at the bottom of a well and determining a background value; another method is to place a at r from the well head and change its orientation to the borehole, make primary and secondary induced polarization measurements in the well for each different a pole orientation, called earth-well mode orientation measurements, for ascertaining the well-side blind mine and determining its spatial location, and earth-well mode operation for ascertaining the well-side blind mine and determining its spatial location, ascertaining the well-bottom blind mine, determining the background value.

Preferably, the well-to-ground operation modes are divided into well-to-place profile measurements and well-to-place laser depths.

Preferably, the well-local profile measurement comprises: the electrode is placed at a selected depth in the well, the other electrode is arranged on the ground at infinity, and the measuring electrode MN is arranged on the ground and measures along a measuring line, including cross section and longitudinal section measurement and vector measurement.

Preferably, the well-local induced electrical sounding comprises: the method comprises the steps of placing a power supply electrode in a well, enabling the other electrode to be located on the ground at infinity, changing the depth of the power supply electrode point by point, fixing measuring electrodes M and N to a well mouth for observation at a certain distance, and enabling the well-local induced polarization depth measurement to be used for tracking the trend of an ore body and judging the occurrence factor of the ore body.

Preferably, the well-to-well pattern arrangement apparatus is divided into 2 types: the single well-well mode and the double well-well mode place the power supply device and the measuring device in the same borehole, and comprise induced polarization logging and intermediate gradient in the single well; in the twin-well method, the power supply device is placed in one borehole, and the measuring device is placed in the other borehole, so that work can be performed only by simultaneously having two boreholes.

Preferably, the induced polarization logging is used for dividing a drilling geological profile and determining an induced electrical property parameter.

Preferably, the well-to-well excitation curve generated by the well-to-well method comprises:

(1) unipolar fixed power supply arrangement: generating big upper, right and lower negative exceptions, wherein the position of the zero value point corresponds to the burial depth of the right end of the ore body;

(2) intermediate gradient arrangement: the curve amplitude is not large, and the position of the maximum value corresponds to the burial depth of the right end of the ore body;

(3) bipolar synchronous alignment: the curve amplitude is large, and the position of the maximum value corresponds to the buried depth of the right end of the ore body.

The invention has the beneficial effects that: and (3) carrying out induced polarization measurement by an in-well induced polarization method, and determining the abnormal change of the polarizability at the position of the ore body and the position of the non-ore body to estimate the ore body extending condition. Through the extending direction that can more effectual discernment deep manganese ore body at ore body excitation power field, measurement accuracy is high.

The above and other objects, advantages and features of the present invention will become more apparent to those skilled in the art from the following detailed description of specific embodiments thereof, taken in conjunction with the accompanying drawings.

Drawings

FIG. 1 shows a flow chart of a method for identifying a latently deposited manganese-rich ore according to an embodiment of the invention;

FIG. 2 is a schematic representation of earth-well operation according to an embodiment of the present invention;

FIG. 3 shows a graph of the spherical secondary field potential difference according to an embodiment of the invention;

FIG. 4 shows a chart relating an induced electrical log and a surface induced electrical measurement according to an embodiment of the invention;

FIG. 5 is a schematic diagram illustrating an arbitrary tangent method for a geowell induced electrical measurement mode according to an embodiment of the present invention;

FIG. 6 is a schematic diagram illustrating a formation-well induced electrical measurement in accordance with an embodiment of the present invention;

fig. 7(a) - (d) are schematic diagrams respectively illustrating the twin-well induced electromotive resistivity mode of the fixed single-plate power supply mobile bipolar measurement, the fixed bipolar power supply mobile bipolar measurement, the middle gradient arrangement, the bipolar power supply bipolar measurement and the like which move synchronously in the same depth according to the embodiment of the invention;

fig. 8 shows a schematic view of an experiment of a well-well model copper plate according to an embodiment of the present invention.

Detailed Description

The well induced polarization method (well induced polarization for short) is a general name of various working modes for induced polarization measurement in a borehole, and the well induced polarization has increasingly wide application in the exploration of copper ores, multi-metal ores and certain weak magnetic or nonmagnetic iron ores at home and abroad. The well induced electricity is characterized in that:

(1) the field source or the receiving equipment is arranged underground, so that the instrument approaches or penetrates through an ore body from different depths and different directions, and the capability of detecting the depth and finding a deep ore is effectively improved;

(2) the flexible working mode is convenient for searching blind mines beside and at the bottom of the well, and determining the burial depth, connectivity, spreading range, attitude and the like of an ore body;

(3) and the field source and the observation device are arranged in the well, so that the influence of terrain and surface unevenness is reduced.

The method for identifying the blind sedimentary manganese-rich ore comprises the following steps:

step 1, measuring abnormal change of enclosed polarizability at the position of an ore body by induced polarization in a well;

step 2, measuring abnormal change of the delineation polarizability at a non-mine position by induced polarization in a well;

and 3, inferring the extension condition of the ore-enriched body by delineating the abnormal changes of the polarizability at the position of the ore body and the position of the non-ore body, and further identifying the hidden sedimentary manganese-enriched ore.

At present, the related exploration specifications represented by rare earth metal geological exploration specification (DZ/T0204-.

The induced polarization method induced polarization measurement in the well in the step 1 and the step 2 comprises an earth-well working mode, a well-earth working mode and a well-well working mode.

Referring to fig. 2, the earth-well mode of operation includes two arrangements: one is to use a metal casing as a power supply electrode a, namely, a so-called wellhead grounding-well mode (r is 0), which can be used for finding blind mines at the bottom of a well and determining a background value; another method is to place a at r from the well head and change its orientation to the borehole, and make primary and secondary induced polarization measurements in the well for each different a-pole orientation, called earth-well mode orientation measurements, to pinpoint the blind side of the well and determine its spatial location. The earth-well working mode is mainly used for finding out blind mines beside a well and determining the spatial position of the blind mines, finding out blind mines at the bottom of the well, determining a background value and the like.

1. Judging the position of the ore body:

as shown in fig. 3, the main orientation is r 100 in this embodiment, the orientation of the sphere is, the opposite orientation is r-100, and the sleeve ground r is 03 in the secondary field potential difference curve of the sphere. When the orientation is dominant, the sphere is nearly vertically polarized, the potential difference amplitude of the secondary field is the largest, the curve form is reverse S-shaped, and the sphere center is positioned between the maximum value and the second zero point; when the orientation is reversed, the sphere is close to horizontal polarization, the amplitude is minimum, the secondary field potential difference curve form is a positive S shape, and the sphere center position is between the maximum value and the first zero point value; when the sleeve is grounded, the sphere is nearly vertically polarized, the secondary field potential difference curve form is nearly symmetrical, and the sphere center is between the maximum value and the first zero value. Therefore, the orientation of the sphere relative to the borehole can be determined according to the shape and the amplitude of the quadratic field potential difference curve.

Fig. 4 shows the electro-stimulation measurement results of the electro-stimulation well and the earth well of a certain blind sedimentary manganese-rich ore in the embodiment. The ZK109 hole has no industrial ore body, and the logging result shows that the upper part has high resistance and low polarizability, and the lower part (the hole depth is less than 40 m) has low resistance and high polarizability, and is mainly sulfide mineralized sandstone. The earth-well mode power supply electrode A measures a reaction background field at a wellhead r-0, and the polarizability of 4 azimuths (55 degrees, 150 degrees, 230 degrees and 265 degrees) excited by the earth-well mode indicates that the azimuths are the maximum reaction amplitude, and the curve is in an inverse S shape, so that the fact that the ore body is positioned on the south side of the ZK109 well and the azimuths are 150 degrees is inferred, and then the result is verified by drilling, and the reference is shown in FIG. 4.

2. Forecasting blind mine at bottom of well

The bottom hole forecast blind mine adopts the ground well mode of r 0 or r 50m to excite electricity to measure, when the bottom hole has blind mine, the apparent polarization rate or the secondary field potential difference abnormal curve has positive or negative opening abnormality. Estimating the apparent polarizability or the secondary field potential difference abnormal curve by adopting an arbitrary tangent method, wherein the estimation comprises the following steps: randomly selecting a point C ' on the view polarizability or secondary field potential difference abnormal curve, performing well axis projection on the point C ' to obtain C as a tangent line of the point C ', intersecting the point d at the well axis, drawing a circle by taking C as the center of the circle and cd as the radius to obtain the position of the mine roof, as shown in FIG. 5.

Preferably, the well-to-ground operation modes are divided into well-to-place profile measurements and well-to-place laser depths.

1. Well-local profile measurement

As shown in fig. 6, the a pole is placed at a selected depth in the well, B is at the ground at infinity, and the measuring electrode MN is laid on the ground to measure along the measuring line, which can also be called a sinking electrode or buried electrode method, including cross section and longitudinal section measurement, and vector measurement. The method is mainly used for tracing the trend of the ore body, judging the state of the ore body and the like.

2. Well-local type laser sounding

The power supply electrode A is placed in a well, the depth of the power supply electrode A is changed point by point on the ground at infinity, and the measuring electrodes M and N are fixed at a certain distance of a well mouth for observation and are mainly used for forecasting blind mines at the bottom of the well.

The well-local is factors of electric shock tracing of ore body trend, ore body occurrence judgment and the like, and the factors mainly comprise maximum, minimum, zero and half-amplitude points according to the power source position in the well, the ore body position, the ore body shape, a ground observation potential curve, a potential gradient curve, abnormal shapes, amplitudes, characteristic points and the like of a secondary field point potential difference curve.

The well-to-well type arrangement device is divided into 2 types: in the single well-well mode, the power supply device and the measuring device are placed in the same borehole, and the methods belonging to the category include induced polarization logging, intermediate gradient in a single well, and the like, as shown in fig. 7, in the double well-well mode, the power supply device is placed in one borehole, and the measuring device is placed in another borehole, and the operation can be carried out only when two boreholes are needed.

Single well-to-well modes, such as induced polarization logging, are used to partition the borehole geological profile and determine the induced electrical property parameters.

As shown in fig. 8, the results of the copper plate model test are well-to-well induced voltage curves of 3 arrangements.

(1) Unipolar fixed power supply arrangement: a1 fixed point power supply, MN mobile measurement, because A1 is near the ore body, the intensity of the polarized field is large, so the large upper and lower negative abnormity is generated, the position of the zero point corresponds to the buried depth of the right end of the ore body.

(2) Intermediate gradient arrangement: the A3B3 supplies power, MN moves and measures, because A3B3 is far away from the ore body, the intensity of the polarized field is small, so the curve amplitude is not large, and the position of the maximum value corresponds to the buried depth of the right end of the ore body.

(3) Bipolar synchronous alignment: the power supply electrode A2B2 and MN measure synchronously, and because the intensity of the polarized field is the largest when the midpoint of A2B2 is opposite to the left end of the ore body, the curve amplitude is large, and the position of the maximum corresponds to the buried depth of the right end of the ore body.

Comparison of the 3 curves shows that bipolar synchro-alignment anomalies are most pronounced, with positive anomalies of about twice the magnitude of the well's median gradient.

In the embodiment, the induced polarization method in the well is used for carrying out induced polarization measurement, and the abnormal change of the polarizability at the position of an ore body and the position of a non-ore body is determined to infer the ore body extending condition. Through the extending direction that can more effectual discernment deep manganese ore body at ore body excitation power field, measurement accuracy is high.

While the present invention has been described with reference to the particular illustrative embodiments, it is not to be restricted by the embodiments but only by the appended claims. It will be understood by those skilled in the art that variations and modifications of the embodiments of the present invention can be made without departing from the scope and spirit of the invention.