Pressure solution–dissolution imparted strike–slip movement: a case study from the Khyber Limestone, Pakistan
Bedding parallel stylolites (BPS), N–S trending microscopic to macroscopic normal faults, and N–S trending calcite-filled veins in the E–W trending Early Devonian Khyber Limestone are synchronously formed as a consequence of vertical shortening. Veins, early stylolite surfaces, and flow folds that o...
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| Veröffentlicht in: | Arabian journal of geosciences 2019-05, Vol.12 (10), p.1-10, Article 327 |
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| creator | Ali, Asghar Khan, Naveed Ahmad, Sohaib Ahmad, Rafique |
| description | Bedding parallel stylolites (BPS), N–S trending microscopic to macroscopic normal faults, and N–S trending calcite-filled veins in the E–W trending Early Devonian Khyber Limestone are synchronously formed as a consequence of vertical shortening. Veins, early stylolite surfaces, and flow folds that oriented oblique to stylolite surfaces have been dissolved in a way that they appear to be displaced by a fault with a strike–slip components. These apparent strike–slip movements along the younger stylolite surfaces have been imparted by selective pressure dissolution of the oblique calcite-filled veins in the Khyber Limestone. The concentration of insoluble residue along the stylolite interface has also facilitated strike–slip movement in an opposite direction to apparent displaced by pressure dissolution. Crosscutting relationship of calcite-filled veins and BPS led to distinguish at least two generations of vein and stylolite formation across the region. |
| doi_str_mv | 10.1007/s12517-019-4499-5 |
| format | Article |
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Veins, early stylolite surfaces, and flow folds that oriented oblique to stylolite surfaces have been dissolved in a way that they appear to be displaced by a fault with a strike–slip components. These apparent strike–slip movements along the younger stylolite surfaces have been imparted by selective pressure dissolution of the oblique calcite-filled veins in the Khyber Limestone. The concentration of insoluble residue along the stylolite interface has also facilitated strike–slip movement in an opposite direction to apparent displaced by pressure dissolution. 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Crosscutting relationship of calcite-filled veins and BPS led to distinguish at least two generations of vein and stylolite formation across the region.</description><subject>Calcite</subject><subject>Case studies</subject><subject>Devonian</subject><subject>Dissolution</subject><subject>Dissolving</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Limestone</subject><subject>Original Paper</subject><subject>Pressure</subject><subject>Slip</subject><issn>1866-7511</issn><issn>1866-7538</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1kMlOwzAQhiMEEqXwANwscSVgu_ESbqhiE5XoAc6Wm0yo2yZpPQ5Sb7wDb8iT4CosJ04zo_n_Wb4kOWX0glGqLpFxwVRKWZ5mWZ6nYi8ZMC1lqsRI7__mjB0mR4gLSqWmSg-SzdQDYueBYLvqgmubz_eP0uFPRVy9tj5ASTB4t4TYxZVbk7p9gxqacEUsKSxGe-jKLal8W5MwB_I4387Ak4mrAUPbwDmZ2qXDYJvj5KCyK4ST7zhMXm5vnsf36eTp7mF8PUkLLnVIy1leSZ4VKj6Q0RxmqhQCFAerc7A0Y6XMR1WlqQRaZcCFYgJECZDzDATw0TA56-eufbvp4hVm0Xa-iSsN51xmWlBOo4r1qsK3iB4qs_autn5rGDU7sqYnayJZsyNrRPTw3oNR27yC_5v8v-kL_Md_ug</recordid><startdate>20190501</startdate><enddate>20190501</enddate><creator>Ali, Asghar</creator><creator>Khan, Naveed</creator><creator>Ahmad, Sohaib</creator><creator>Ahmad, Rafique</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20190501</creationdate><title>Pressure solution–dissolution imparted strike–slip movement: a case study from the Khyber Limestone, Pakistan</title><author>Ali, Asghar ; Khan, Naveed ; Ahmad, Sohaib ; Ahmad, Rafique</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c268t-db9f624c7753409eb7d55e72ea89ea041d693ff806e0f4e25715e5dee924e5e23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Calcite</topic><topic>Case studies</topic><topic>Devonian</topic><topic>Dissolution</topic><topic>Dissolving</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Limestone</topic><topic>Original Paper</topic><topic>Pressure</topic><topic>Slip</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ali, Asghar</creatorcontrib><creatorcontrib>Khan, Naveed</creatorcontrib><creatorcontrib>Ahmad, Sohaib</creatorcontrib><creatorcontrib>Ahmad, Rafique</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Arabian journal of geosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ali, Asghar</au><au>Khan, Naveed</au><au>Ahmad, Sohaib</au><au>Ahmad, Rafique</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Pressure solution–dissolution imparted strike–slip movement: a case study from the Khyber Limestone, Pakistan</atitle><jtitle>Arabian journal of geosciences</jtitle><stitle>Arab J Geosci</stitle><date>2019-05-01</date><risdate>2019</risdate><volume>12</volume><issue>10</issue><spage>1</spage><epage>10</epage><pages>1-10</pages><artnum>327</artnum><issn>1866-7511</issn><eissn>1866-7538</eissn><abstract>Bedding parallel stylolites (BPS), N–S trending microscopic to macroscopic normal faults, and N–S trending calcite-filled veins in the E–W trending Early Devonian Khyber Limestone are synchronously formed as a consequence of vertical shortening. 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| subjects | Calcite Case studies Devonian Dissolution Dissolving Earth and Environmental Science Earth science Earth Sciences Limestone Original Paper Pressure Slip |
| title | Pressure solution–dissolution imparted strike–slip movement: a case study from the Khyber Limestone, Pakistan |
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